1.1
217676
1888010461
info:srw/schema/1/example-v1.1
xml:ISO19139:F
wdc-climate.de:3529778
eng; USA
collection
CMAQ_CCLM_HZG_2008
Dr. Daniel Neumann
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
Volker Matthias
Max-Planck-Institut fuer Meteorologie
http://www.mpimet.mpg.de/
pointOfContact
2017-06-08T08:47:22
ISO 19115
ISO 19115-2:2009
Concentrations of gaseous pollutants and particulate compounds over Northwestern Europe and nitrogen deposition into the North and Baltic Sea in 2008
2017-12-08
publication
1
CMAQ_CCLM_HZG_2008
doi:10.1594/WDCC/CMAQ_CCLM_HZG_2008
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: armin.aulinger@hzg.de
principalInvestigator
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
principalInvestigator
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: johannes.bieser@hzg.de
principalInvestigator
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: volker.matthias@hzg.de
principalInvestigator
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
author
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: volker.matthias@hzg.de
author
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: johannes.bieser@hzg.de
author
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
not filled
Email: armin.aulinger@hzg.de
author
WDC Climate at DKRZ
publisher
The concentrations and deposition of atmospheric constituents such as air pollutants were modeled with the Community Multiscale Air Quality (CMAQ) Model system for the year 2008. A focus was on sea salt emissions, atmospheric sea salt concentrations and the interaction between sea salt particles and atmospheric nitrogen compounds. For this purpose, two model runs with different realistic sea salt emission parameterizations were performed and are provided here. The model run CMAQ_CD24_seasalt_base uses the default sea salt emission parameterization of CMAQ denoted as GO03. The model run CMAQ_CD24_seasalt_ov14 uses an alternative sea salt emission parameterization denoted as OV14. Please refer to the connected references for information on the two sea salt emission parameterizations and their implementation.
The dataset also contains meteorological input parameters in order to allow the user to perform unit conversions for some model variables. Additionally, the land-sea mask and land fraction data per model grid cell are provided.
The projection is a Lambert Conformal Conic projection. The parameters are given in the netCDF files.
Volker Matthias
Max-Planck-Institut fuer Meteorologie
http://www.mpimet.mpg.de/
pointOfContact
NetCDF
aerosol
air pollution
air quality
atmospheric chemistry
chemistry transport modeling
coastdat
sea salt
CC BY 4.0: Creative Commons Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/
eng; USA
18.9
36.9
42.6
67.0
calendrical
2008-01-01
2008-12-31
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
air_density
[CF-Standard Name]; unit: kg m-3
humidity_mixing_ratio
Humidity mixing ratio of a parcel of moist air is the ratio of the mass of water vapor to the mass of dry air. [CF-Standard Name]; unit: 1
air_pressure
air_pressure [CF-Standard Name]; unit: Pa
mass_concentration_of_nitric_acid_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitric acid is HNO3. [CF-Standard Name]; unit: kg m-3
lwe_thickness_of_convective_precipitation_amount
lwe_thickness_of_convective_precipitation_amount [CF-Standard Name]; unit: m
air_pressure
air_pressure [CF-Standard Name]; unit: Pa
air_density
[CF-Standard Name]; unit: kg m-3
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
alias: mass_concentration_of_nitrate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the nitrate anion is NO3-. [CF-Standard Name]; unit: kg m-3
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
Mass fraction is used in the construction "mass_fraction_of_X_in_Y", where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The phrase "sea_salt_cation" is the term used in standard names to describe collectively the group of cationic species that occur in sea salt. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Sea salt cations are mainly sodium (Na+), but also include potassium (K+), magnesium (Mg2+), calcium (Ca2+) and rarer cations. Where possible, the data variable should be accompanied by a complete description of the ions represented, for example, by using a comment attribute. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ozone_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ozone is O3. [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
Mass fraction is used in the construction "mass_fraction_of_X_in_Y", where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The phrase "sea_salt_cation" is the term used in standard names to describe collectively the group of cationic species that occur in sea salt. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Sea salt cations are mainly sodium (Na+), but also include potassium (K+), magnesium (Mg2+), calcium (Ca2+) and rarer cations. Where possible, the data variable should be accompanied by a complete description of the ions represented, for example, by using a comment attribute. [CF-Standard Name]; unit: kg m-3
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_nitrogen_dioxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen dioxide is NO2. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfur_dioxide_in_air
[CF-Standard Name]; unit: kg m-3
humidity_mixing_ratio
Humidity mixing ratio of a parcel of moist air is the ratio of the mass of water vapor to the mass of dry air. [CF-Standard Name]; unit: 1
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
alias: mass_concentration_of_sulfate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the sulfate anion is SO4(2-). [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen dioxide is NO2. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen dioxide is NO2. [CF-Standard Name]; unit: kg m-3
humidity_mixing_ratio
Humidity mixing ratio of a parcel of moist air is the ratio of the mass of water vapor to the mass of dry air. [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_ozone_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ozone is O3. [CF-Standard Name]; unit: kg m-3
air_density
[CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
alias: mass_concentration_of_sulfate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the sulfate anion is SO4(2-). [CF-Standard Name]; unit: kg m-3
lwe_thickness_of_stratiform_precipitation_amount
alias: lwe_thickness_of_large_scale_precipitation_amount
The construction lwe_thickness_of_X_amount or _content means the vertical extent of a layer of liquid water having the same mass per unit area. Stratiform precipitation, whether liquid or frozen, is precipitation that formed in stratiform cloud. "Precipitation" in the earth's atmosphere means precipitation of water in all phases. The abbreviation "lwe" means liquid water equivalent. [CF-Standard Name]; unit: m
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
alias: mass_concentration_of_ammonium_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for ammonium is NH4. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ammonia_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ammonia is NH3. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
alias: mass_concentration_of_sulfate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the sulfate anion is SO4(2-). [CF-Standard Name]; unit: kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
not filled; unit: kg m-3
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
lwe_thickness_of_convective_precipitation_amount
lwe_thickness_of_convective_precipitation_amount [CF-Standard Name]; unit: m
mass_concentration_of_ammonia_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ammonia is NH3. [CF-Standard Name]; unit: kg m-3
lwe_thickness_of_stratiform_precipitation_amount
alias: lwe_thickness_of_large_scale_precipitation_amount
The construction lwe_thickness_of_X_amount or _content means the vertical extent of a layer of liquid water having the same mass per unit area. Stratiform precipitation, whether liquid or frozen, is precipitation that formed in stratiform cloud. "Precipitation" in the earth's atmosphere means precipitation of water in all phases. The abbreviation "lwe" means liquid water equivalent. [CF-Standard Name]; unit: m
mass_concentration_of_nitrogen_monoxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen monoxide is NO. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
alias: mass_concentration_of_ammonium_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for ammonium is NH4. [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_nitric_acid_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitric acid is HNO3. [CF-Standard Name]; unit: kg m-3
air_pressure
air_pressure [CF-Standard Name]; unit: Pa
mass_concentration_of_nitric_acid_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitric acid is HNO3. [CF-Standard Name]; unit: kg m-3
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
Mass fraction is used in the construction "mass_fraction_of_X_in_Y", where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The phrase "sea_salt_cation" is the term used in standard names to describe collectively the group of cationic species that occur in sea salt. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Sea salt cations are mainly sodium (Na+), but also include potassium (K+), magnesium (Mg2+), calcium (Ca2+) and rarer cations. Where possible, the data variable should be accompanied by a complete description of the ions represented, for example, by using a comment attribute. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen monoxide is NO. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitric_acid_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitric acid is HNO3. [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
alias: mass_concentration_of_nitrate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the nitrate anion is NO3-. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
not filled; unit: kg m-3
mass_concentration_of_sulfur_dioxide_in_air
[CF-Standard Name]; unit: kg m-3
mass_concentration_of_ozone_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ozone is O3. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen monoxide is NO. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen dioxide is NO2. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ozone_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ozone is O3. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ammonia_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ammonia is NH3. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfur_dioxide_in_air
[CF-Standard Name]; unit: kg m-3
lwe_thickness_of_convective_precipitation_amount
lwe_thickness_of_convective_precipitation_amount [CF-Standard Name]; unit: m
lwe_thickness_of_stratiform_precipitation_amount
alias: lwe_thickness_of_large_scale_precipitation_amount
The construction lwe_thickness_of_X_amount or _content means the vertical extent of a layer of liquid water having the same mass per unit area. Stratiform precipitation, whether liquid or frozen, is precipitation that formed in stratiform cloud. "Precipitation" in the earth's atmosphere means precipitation of water in all phases. The abbreviation "lwe" means liquid water equivalent. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
lwe_thickness_of_convective_precipitation_amount
lwe_thickness_of_convective_precipitation_amount [CF-Standard Name]; unit: m
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
alias: mass_concentration_of_nitrate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the nitrate anion is NO3-. [CF-Standard Name]; unit: kg m-3
air_pressure
air_pressure [CF-Standard Name]; unit: Pa
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
alias: mass_concentration_of_ammonium_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for ammonium is NH4. [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfur_dioxide_in_air
[CF-Standard Name]; unit: kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
alias: mass_concentration_of_ammonium_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for ammonium is NH4. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_ammonia_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ammonia is NH3. [CF-Standard Name]; unit: kg m-3
lwe_thickness_of_stratiform_precipitation_amount
alias: lwe_thickness_of_large_scale_precipitation_amount
The construction lwe_thickness_of_X_amount or _content means the vertical extent of a layer of liquid water having the same mass per unit area. Stratiform precipitation, whether liquid or frozen, is precipitation that formed in stratiform cloud. "Precipitation" in the earth's atmosphere means precipitation of water in all phases. The abbreviation "lwe" means liquid water equivalent. [CF-Standard Name]; unit: m
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
Mass fraction is used in the construction "mass_fraction_of_X_in_Y", where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The phrase "sea_salt_cation" is the term used in standard names to describe collectively the group of cationic species that occur in sea salt. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Sea salt cations are mainly sodium (Na+), but also include potassium (K+), magnesium (Mg2+), calcium (Ca2+) and rarer cations. Where possible, the data variable should be accompanied by a complete description of the ions represented, for example, by using a comment attribute. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
alias: mass_concentration_of_nitrate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the nitrate anion is NO3-. [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_chloride_dry_aerosol_particles_in_air
not filled; unit: kg m-3
air_density
[CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
alias: mass_concentration_of_sulfate_dry_aerosol_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. "Dry aerosol particles" means aerosol particles without any water uptake. The chemical formula for the sulfate anion is SO4(2-). [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_nitrogen_monoxide_in_air
Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for nitrogen monoxide is NO. [CF-Standard Name]; unit: kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
not filled; unit: kg m-3
humidity_mixing_ratio
Humidity mixing ratio of a parcel of moist air is the ratio of the mass of water vapor to the mass of dry air. [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Wet deposition" means deposition by precipitation. "Oxidized nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state greater than zero. Usually, particle bound and gaseous nitrogen compounds, such as nitrogen monoxide (NO), nitrogen dioxide (NO2), dinitrogen pentoxide (N2O5), nitric acid (HNO3), nitrate (NO3-), peroxynitric acid (HNO4), bromine nitrate (BrONO2), chlorine nitrate (ClONO2) and organic nitrates (most notably peroxyacetyl nitrate, sometimes referred to as PAN, (CH3COO2NO2)), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Dry deposition" is the sum of turbulent deposition and gravitational settling. "Reduced nitrogen compounds" means all chemical species containing nitrogen atoms with an oxidation state less than zero. Usually, particle bound and gaseous nitrogen compounds, primarily ammonium (NH4+) and ammonia (NH3), are included. The list of individual species that are included in this quantity can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. [CF-Standard Name]; unit: kg m-2 s-1
NetCDF
12459
https://www.wdc-climate.de/ui/entry?acronym=CMAQ_CCLM_HZG_2008
information
collection
n/a
None
n/a
None
]]>
1
info:srw/schema/1/example-v1.1
xml:ISO19139:F
wdc-climate.de:3453649
eng; USA
collection
GMG5DEC
Dr. Michael Lautenschlager
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
Siegfried Schubert
NASA Goddard Institute for Space Studies
http://www.giss.nasa.gov/
pointOfContact
2014-07-10T09:51:44
ISO 19115
ISO 19115-2:2009
GEOS-5 model output prepared for CMIP5 decadal experiments, served by ESGF
2015-02-03
publication
1
GMG5DEC
doi:10.1594/WDCC/CMIP5.GMG5DEC
Siegfried Schubert
NASA Goddard Institute for Space Studies
http://www.giss.nasa.gov/
Email: Siegfried.D.Schubert@nasa.gov
principalInvestigator
Siegfried Schubert
NASA Goddard Institute for Space Studies
http://www.giss.nasa.gov/
Email: Siegfried.D.Schubert@nasa.gov
author
WDC Climate at DKRZ
publisher
decadals are a group of experiments of the CMIP5 - Coupled Model Intercomparison Project Phase 5 ( https://pcmdi.llnl.gov/mips/cmip5 ). CMIP5 is meant to provide a framework for coordinated climate change experiments for the next five years and thus includes simulations for assessment in the AR5 as well as others that extend beyond the AR5.
1.5 decadal (1.5 decadal hindcast/forecast utilizing alternative initializations.) - Version 1: Decadal hindcast/prediction. Comparison of initialization strategies - for example, a repeat of experiment 1.1 using an alternate initialization strategy or alternate initial data. Individual decadal experiments are named decadalXXXX with starting year XXXX.
Experiment design: https://pcmdi.llnl.gov/mips/cmip5/experiment_design.html
List of output variables: https://pcmdi.llnl.gov/mips/cmip5/datadescription.html
Output: time series per variable in model grid spatial resolution in netCDF format
Earth System model and the simulation information: CIM repository
Entry name/title of data are specified according to the Data Reference Syntax ( https://pcmdi.llnl.gov/mips/cmip5/docs/cmip5_data_reference_syntax.pdf ) as activity/product/institute/model/experiment/frequency/modeling realm/MIP table/ensemble member/version number/variable name/CMOR filename.nc .
Siegfried Schubert
NASA Goddard Institute for Space Studies
http://www.giss.nasa.gov/
pointOfContact
NetCDF
CMIP5
GEOS-5
IPCC
IPCC-AR5
IPCC-DDC
WGI
climate simulation
decadals
unrestricted: unrestricted
eng; USA
0.0
360.0
-90.0
90.0
proleptic_gregorian
1961-01-01
2019-12-31
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_cloud_ice
Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_cloud_ice
Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
soil_moisture_content
"moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_in_air
Surface Concentration of Dry Aerosol Primary Organic Matter [CF-Standard Name]; unit: kg m-3
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_dimethyl_sulfide_in_air
mole_fraction_of_dimethyl_sulfide_in_air [CF-Standard Name]; unit: 1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_sulfur_dioxide_in_air
mole_fraction_of_sulfur_dioxide_in_air [CF-Standard Name]; unit: 1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_emission
[CF-Standard Name]; unit: kg m-2 s-1
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_downward_heat_flux_in_snow
surface_downward_heat_flux_in_snow [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except black carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
NetCDF
2747320
https://www.wdc-climate.de/ui/entry?acronym=GMG5DEC
information
collection
]]>
2
info:srw/schema/1/example-v1.1
xml:ISO19139:F
de.dkrz.wdcc.iso2320276
series
MIM5c2
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
author
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
pointOfContact
Prof. Masahiro Watanabe
Center for Climate System Research, The University of Tokyo
http://www.ccsr.u-tokyo.ac.jp/
originator
Dr. Seita Emori
National Institute for Environmental Studies
http://www.nies.go.jp/index-e.html
originator
2019-04-21T04:21:11
ISO 19115
ISO 19139 / DKRZ ISO Simple Profile V1.0
http://doi.org/doi:10.1594/WDCC/CMIP5.MIM5c2
cmip5 output1 MIROC MIROC5 abrupt4xCO2
cmip5 output1 MIROC MIROC5 abrupt4xCO2
2012-01-13
creation
None
MIROC5 model output prepared for CMIP5 abrupt4xCO2, served by ESGF
doi:10.1594/WDCC/CMIP5.MIM5c2
Prof. Masahiro Watanabe
Center for Climate System Research, The University of Tokyo
http://www.ccsr.u-tokyo.ac.jp/
originator
Dr. Seita Emori
National Institute for Environmental Studies
http://www.nies.go.jp/index-e.html
originator
doi:10.1594/WDCC/CMIP5.MIM5c2
'abrupt4xco2' is an experiment of the CMIP5 - Coupled Model Intercomparison Project Phase 5
(https://pcmdi.llnl.gov/mips/cmip5). CMIP5 is meant to provide a framework for coordinated
climate change experiments for the next five years and thus includes simulations for
assessment in the AR5 as well as others that extend beyond the AR5.
6.3 abrupt4xco2 (6.3 Abrupt 4XCO2) - Version 1: Impose an instantaneous quadrupling of CO2, then hold fixed.
Experiment design: https://pcmdi.llnl.gov/mips/cmip5/experiment_design.html
List of output variables: https://pcmdi.llnl.gov/mips/cmip5/datadescription.html
Output: time series per variable in model grid spatial resolution in netCDF format
Earth System model and the simulation information: CIM repository
Entry name/title of data are specified according to the Data Reference Syntax
(https://pcmdi.llnl.gov/mips/cmip5/docs/cmip5_data_reference_syntax.pdf)
as activity/product/institute/model/experiment/frequency/modeling realm/MIP table/ensemble
member/version number/variable name/CMOR filename.nc.
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
author
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
pointOfContact
IPCC
theme
climate simulation
theme
MIROC5
theme
IPCC-AR5
theme
CMIP5
theme
IPCC-DDC
theme
eng
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modelResult
0.01
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modelResult
0.01
area_fraction
modelResult
0.01
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modelResult
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modelResult
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
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1
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modelResult
1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
modelResult
1
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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kg m-2
atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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atmosphere_cloud_condensed_water_content
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atmosphere_mass_content_of_cloud_ice
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atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_cloud_ice
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kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
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kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
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kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
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kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_dust_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_seasalt_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
modelResult
kg m-2
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_mass_of_carbon_dioxide
modelResult
kg
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
modelResult
kg m-2 s-1
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_number_content_of_cloud_droplets
modelResult
m-2
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
modelResult
1
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
atmosphere_water_vapor_content
modelResult
kg m-2
cell_area
modelResult
m2
cell_area
modelResult
m2
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cell_thickness
modelResult
m
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_albedo
modelResult
1
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
cloud_area_fraction_in_atmosphere_layer
modelResult
0.01
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
convective_precipitation_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
downward_sea_ice_basal_salt_flux
modelResult
kg m-2 s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
eastward_wind
modelResult
m s-1
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_convective_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
effective_radius_of_stratiform_cloud_liquid_water_particle
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
geopotential_height
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_steric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
global_average_thermosteric_sea_level_change
modelResult
m
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
W m-2
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
isccp_cloud_area_fraction
modelResult
0.01
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
lagrangian_tendency_of_air_pressure
modelResult
Pa s-1
land_area_fraction
modelResult
0.01
land_ice_area_fraction
modelResult
0.01
leaf_area_index
modelResult
1
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_dust_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_in_air
modelResult
kg m-3
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_ice_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
mass_fraction_of_cloud_liquid_water_in_air
modelResult
1
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
moisture_content_of_soil_layer
modelResult
kg m-2
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_dimethyl_sulfide_in_air
modelResult
1
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_methane_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_nitrous_oxide_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_ozone_in_air
modelResult
1e-9
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
mole_fraction_of_sulfur_dioxide_in_air
modelResult
1
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
modelResult
W m-2
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_ambient_aerosol_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
modelResult
m-3
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_mixed_layer_thickness_defined_by_mixing_scheme
modelResult
m
ocean_volume
modelResult
m3
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
precipitation_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
rainfall_flux
modelResult
kg m-2 s-1
region
modelResult
1
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
relative_humidity
modelResult
0.01
root_depth
modelResult
m
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
runoff_flux
modelResult
kg m-2 s-1
sea_area_fraction
modelResult
0.01
sea_floor_depth_below_geoid
modelResult
m
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_and_surface_snow_amount
modelResult
kg m-2
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_area_fraction
modelResult
0.01
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_salinity
modelResult
psu
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_surface_temperature
modelResult
K
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_thickness
modelResult
m
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_transport
modelResult
kg s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_x_velocity
modelResult
m s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_transport
modelResult
kg s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_ice_y_velocity
modelResult
m s-1
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_height_above_geoid
modelResult
m
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_salinity
modelResult
psu
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_surface_temperature
modelResult
K
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass
modelResult
kg
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_mass_per_unit_area
modelResult
kg m-2
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_potential_temperature
modelResult
K
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_pressure_at_sea_floor
modelResult
dbar
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_salinity
modelResult
psu
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_volume
modelResult
m3
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_x_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
sea_water_y_velocity
modelResult
m s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
snowfall_flux
modelResult
kg m-2 s-1
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_frozen_water_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content
modelResult
kg m-2
soil_moisture_content_at_field_capacity
modelResult
kg m-2
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soil_temperature
modelResult
K
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
soot_content_of_surface_snow
modelResult
kg m-2
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
specific_humidity
modelResult
1
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_height_above_geoid
modelResult
m2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_sea_surface_temperature
modelResult
K2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
square_of_upward_ocean_mass_transport
modelResult
kg2 s-2
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_air_pressure
modelResult
Pa
surface_altitude
modelResult
m
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_eastward_stress
modelResult
Pa
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_heat_flux_in_sea_water
modelResult
W m-2
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_northward_stress
modelResult
Pa
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_x_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downward_y_stress
modelResult
N m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_runoff_flux
modelResult
kg m-2 s-1
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_amount
modelResult
kg m-2
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_and_ice_sublimation_flux
modelResult
kg m-2 s-1
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_area_fraction
modelResult
0.01
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_melt_flux
modelResult
kg m-2 s-1
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_snow_thickness
modelResult
m
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_temperature
modelResult
K
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_latent_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upward_sensible_heat_flux
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_longwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
modelResult
W m-2
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
temperature_in_surface_snow
modelResult
K
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
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modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
modelResult
kg m-2 s-1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_bidirectional_reflectance
modelResult
1
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_incoming_shortwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_longwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
toa_outgoing_shortwave_flux_assuming_clear_sky
modelResult
W m-2
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
transpiration_flux
modelResult
kg m-2 s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
upward_ocean_mass_transport
modelResult
kg s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
modelResult
m-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_canopy
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_evaporation_flux_from_soil
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
water_flux_into_sea_water_from_rivers
modelResult
kg m-2 s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
wind_speed
modelResult
m s-1
NetCDF
network Common Data Format
distributor
Mb
2149410
http://doi.org/doi:10.1594/WDCC/CMIP5.MIM5c2
series
]]>
3
info:srw/schema/1/example-v1.1
xml:ISO19139:F
de.dkrz.wdcc.iso3529778
series
CMAQ_CCLM_HZG_2008
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
author
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
pointOfContact
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
originator
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
2022-04-25T05:41:14
ISO 19115
ISO 19139 / DKRZ ISO Simple Profile V1.0
http://doi.org/doi:10.1594/WDCC/CMAQ_CCLM_HZG_2008
Concentrations of gaseous pollutants and particulate compounds over Northwestern Europe and nitrogen deposition into the North and Baltic Sea in 2008
Concentrations of gaseous pollutants and particulate compounds over Northwestern Europe and nitrogen deposition into the North and Baltic Sea in 2008
2017-06-08
creation
None
Concentrations of gaseous pollutants and particulate compounds over Northwestern Europe and nitrogen deposition into the North and Baltic Sea in 2008
doi:10.1594/WDCC/CMAQ_CCLM_HZG_2008
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
originator
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
originator
doi:10.1594/WDCC/CMAQ_CCLM_HZG_2008
The concentrations and deposition of atmospheric constituents such as air pollutants were modeled with the Community Multiscale Air Quality (CMAQ) Model system for the year 2008. A focus was on sea salt emissions, atmospheric sea salt concentrations and the interaction between sea salt particles and atmospheric nitrogen compounds. For this purpose, two model runs with different realistic sea salt emission parameterizations were performed and are provided here. The model run CMAQ_CD24_seasalt_base uses the default sea salt emission parameterization of CMAQ denoted as GO03. The model run CMAQ_CD24_seasalt_ov14 uses an alternative sea salt emission parameterization denoted as OV14. Please refer to the connected references for information on the two sea salt emission parameterizations and their implementation.
The dataset also contains meteorological input parameters in order to allow the user to perform unit conversions for some model variables. Additionally, the land-sea mask and land fraction data per model grid cell are provided.
The projection is a Lambert Conformal Conic projection. The parameters are given in the netCDF files.
Dr. Daniel Neumann
Leibniz-Institut für Ostseeforschung Warnemünde
https://www.io-warnemuende.de/
author
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Dr. Johannes Bieser
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Dr. Armin Aulinger
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
author
Volker Matthias
Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH
pointOfContact
aerosol
theme
atmospheric chemistry
theme
sea salt
theme
air pollution
theme
coastdat
theme
air quality
theme
chemistry transport modeling
theme
eng
18.9
36.9
42.6
67.0
2008-05-17
2008-09-30
137
2008-07-01
2008-09-30
92
2008-01-01
2008-03-31
91
2008-11-15
2008-12-31
47
air_density
modelResult
kg m-3
air_density
modelResult
kg m-3
air_density
modelResult
kg m-3
air_density
modelResult
kg m-3
air_pressure
modelResult
Pa
air_pressure
modelResult
Pa
air_pressure
modelResult
Pa
air_pressure
modelResult
Pa
air_temperature
modelResult
K
air_temperature
modelResult
K
air_temperature
modelResult
K
air_temperature
modelResult
K
humidity_mixing_ratio
modelResult
1
humidity_mixing_ratio
modelResult
1
humidity_mixing_ratio
modelResult
1
humidity_mixing_ratio
modelResult
1
lwe_thickness_of_convective_precipitation_amount
modelResult
m
lwe_thickness_of_convective_precipitation_amount
modelResult
m
lwe_thickness_of_convective_precipitation_amount
modelResult
m
lwe_thickness_of_convective_precipitation_amount
modelResult
m
lwe_thickness_of_stratiform_precipitation_amount
modelResult
m
lwe_thickness_of_stratiform_precipitation_amount
modelResult
m
lwe_thickness_of_stratiform_precipitation_amount
modelResult
m
lwe_thickness_of_stratiform_precipitation_amount
modelResult
m
mass_concentration_of_ammonia_in_air
modelResult
kg m-3
mass_concentration_of_ammonia_in_air
modelResult
kg m-3
mass_concentration_of_ammonia_in_air
modelResult
kg m-3
mass_concentration_of_ammonia_in_air
modelResult
kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_ammonium_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_chloride_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_nitrate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_nitric_acid_in_air
modelResult
kg m-3
mass_concentration_of_nitric_acid_in_air
modelResult
kg m-3
mass_concentration_of_nitric_acid_in_air
modelResult
kg m-3
mass_concentration_of_nitric_acid_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
modelResult
kg m-3
mass_concentration_of_nitrogen_monoxide_in_air
modelResult
kg m-3
mass_concentration_of_ozone_in_air
modelResult
kg m-3
mass_concentration_of_ozone_in_air
modelResult
kg m-3
mass_concentration_of_ozone_in_air
modelResult
kg m-3
mass_concentration_of_ozone_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_sulfate_dry_aerosol_particles_in_air
modelResult
kg m-3
mass_concentration_of_sulfur_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_sulfur_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_sulfur_dioxide_in_air
modelResult
kg m-3
mass_concentration_of_sulfur_dioxide_in_air
modelResult
kg m-3
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
modelResult
kg m-3
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
modelResult
kg m-3
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
modelResult
kg m-3
mass_fraction_of_sea_salt_dry_aerosol_particles_expressed_as_cations_in_air
modelResult
kg m-3
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_oxidized_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
tendency_of_atmosphere_mass_content_of_reduced_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition
modelResult
kg m-2 s-1
NetCDF
network Common Data Format
distributor
Mb
12459
http://doi.org/doi:10.1594/WDCC/CMAQ_CCLM_HZG_2008
series
]]>
4
info:srw/schema/1/example-v1.1
xml:ISO19139:F
wdc-climate.de:3455812
eng; USA
collection
MIM5DEC
Dr. Michael Lautenschlager
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
Dr. Michael Lautenschlager
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
pointOfContact
2014-07-22T15:25:28
ISO 19115
ISO 19115-2:2009
MIROC5 model output prepared for CMIP5 decadals, served by ESGF
2015-01-29
publication
1
MIM5DEC
doi:10.1594/WDCC/CMIP5.MIM5DEC
Prof. Masahiro Watanabe
Center for Climate System Research, The University of Tokyo
http://www.ccsr.u-tokyo.ac.jp/
Email: hiro@aori.u-tokyo.ac.jp
principalInvestigator
Dr. Seita Emori
National Institute for Environmental Studies
http://www.nies.go.jp/index-e.html
Email: emori@nies.go.jp
principalInvestigator
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
Email: hiro@aori.u-tokyo.ac.jp
author
WDC Climate at DKRZ
publisher
decadals are a group of experiments of the CMIP5 - Coupled Model Intercomparison Project Phase 5 ( https://pcmdi.llnl.gov/mips/cmip5 ). CMIP5 is meant to provide a framework for coordinated climate change experiments for the next five years and thus includes simulations for assessment in the AR5 as well as others that extend beyond the AR5.
1.5 decadal (1.5 decadal hindcast/forecast utilizing alternative initializations.) - Version 1: Decadal hindcast/prediction. Comparison of initialization strategies - for example, a repeat of experiment 1.1 using an alternate initialization strategy or alternate initial data. Individual decadal experiments are named decadalXXXX with starting year XXXX.
Experiment design: https://pcmdi.llnl.gov/mips/cmip5/experiment_design.html
List of output variables: https://pcmdi.llnl.gov/mips/cmip5/datadescription.html
Output: time series per variable in model grid spatial resolution in netCDF format
Earth System model and the simulation information: CIM repository
Entry name/title of data are specified according to the Data Reference Syntax ( https://pcmdi.llnl.gov/mips/cmip5/docs/cmip5_data_reference_syntax.pdf ) as activity/product/institute/model/experiment/frequency/modeling realm/MIP table/ensemble member/version number/variable name/CMOR filename.nc .
Prof. Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo
http://www.aori.u-tokyo.ac.jp/english/
pointOfContact
NetCDF
CMIP5
IPCC
IPCC-AR5
IPCC-DDC
MIROC5
WGI
climate simulation
decadals
unrestricted: unrestricted
eng; USA
0.0
360.0
-90.0
90.0
proleptic_gregorian
1960-01-16
2020-12-16
sea_area_fraction
Sea Area Fraction [CF-Standard Name]; unit: 0.01
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
global_average_steric_sea_level_change
Global Average Steric Sea Level Change [CF-Standard Name]; unit: m
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
Heat Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
surface_downward_northward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
soil_frozen_water_content
Soil Frozen Water Content [CF-Standard Name]; unit: kg m-2
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_salinity
The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: psu
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
Heat Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: W m-2
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_eastward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
soil_frozen_water_content
Soil Frozen Water Content [CF-Standard Name]; unit: kg m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_cloud_ice
Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_ice_surface_temperature
sea_ice_surface_temperature [CF-Standard Name]; unit: K
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
soot_content_of_surface_snow
soot_content_of_surface_snow [CF-Standard Name]; unit: kg m-2
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
Heat Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
surface_downward_northward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
[CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
water_flux_into_sea_water
alias: water_flux_into_ocean
"Water" means water in all phases. The water flux into sea water is the freshwater entering as a result of precipitation, evaporation, river inflow, sea ice effects and water flux relaxation and correction (if applied). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
global_average_steric_sea_level_change
Global Average Steric Sea Level Change [CF-Standard Name]; unit: m
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
global_average_steric_sea_level_change
Global Average Steric Sea Level Change [CF-Standard Name]; unit: m
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_downward_northward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux_from_soil
Water means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called sublimation.) In accordance with common usage in geophysical disciplines, flux implies per unit area, called flux density in physics. [CF-Standard Name]; unit: kg m-2 s-1
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
atmosphere_optical_thickness_due_to_pm1_ambient_aerosol
Ambient Fine Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol
Load of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-2
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
sea_ice_and_surface_snow_amount
[CF-Standard Name]; unit: kg m-2
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_cloud_ice
Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
soil_moisture_content
"moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
soil_frozen_water_content
Soil Frozen Water Content [CF-Standard Name]; unit: kg m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
net_downward_radiative_flux_at_top_of_atmosphere_model
Net Downward Flux at Top of Model [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
number_concentration_of_ambient_aerosol_in_air
[CF-Standard Name]; unit: m-3
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water
alias: water_flux_into_ocean
"Water" means water in all phases. The water flux into sea water is the freshwater entering as a result of precipitation, evaporation, river inflow, sea ice effects and water flux relaxation and correction (if applied). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
sea_ice_x_transport
sea_ice_x_transport [CF-Standard Name]; unit: kg s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
number_concentration_of_cloud_liquid_water_particles_in_air
number_concentration_of_cloud_liquid_water_particles_in_air [CF-Standard Name]; unit: m-3
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
water_evaporation_flux_from_soil
Water means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called sublimation.) In accordance with common usage in geophysical disciplines, flux implies per unit area, called flux density in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_mass_content_of_cloud_ice
Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
soil_frozen_water_content
Soil Frozen Water Content [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
toa_outgoing_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
sea_surface_salinity
The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: psu
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
[CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
eastward_sea_water_velocity
sea_water_x_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
[CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
leaf_area_index
"X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
soil_moisture_content
"moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name]; unit: kg m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
soot_content_of_surface_snow
soot_content_of_surface_snow [CF-Standard Name]; unit: kg m-2
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_surface_melting
tendency_of_sea_ice_amount_due_to_surface_melting [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
toa_incoming_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux_from_canopy
Evaporation from Canopy [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
soil_moisture_content
"moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name]; unit: kg m-2
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
sea_ice_surface_temperature
sea_ice_surface_temperature [CF-Standard Name]; unit: K
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_x_transport
sea_ice_x_transport [CF-Standard Name]; unit: kg s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_cloud_condensed_water_content
"condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2
sea_surface_salinity
The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: psu
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
surface_downward_eastward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
sea_surface_height_above_geoid
sea_surface_height_above_geoid [CF-Standard Name]; unit: m
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
number_concentration_of_cloud_liquid_water_particles_in_air
number_concentration_of_cloud_liquid_water_particles_in_air [CF-Standard Name]; unit: m-3
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
soil_moisture_content
"moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name]; unit: kg m-2
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
toa_incoming_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_northward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_water_pressure_at_sea_floor
Sea Water Pressure at Sea floor [CF-Standard Name]; unit: dbar
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
surface_snow_and_ice_sublimation_flux
Sublimation over Sea Ice [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
soot_content_of_surface_snow
soot_content_of_surface_snow [CF-Standard Name]; unit: kg m-2
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_shortwave_flux_assuming_clear_sky
toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
soot_content_of_surface_snow
soot_content_of_surface_snow [CF-Standard Name]; unit: kg m-2
water_flux_into_sea_water
alias: water_flux_into_ocean
"Water" means water in all phases. The water flux into sea water is the freshwater entering as a result of precipitation, evaporation, river inflow, sea ice effects and water flux relaxation and correction (if applied). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_northward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
[CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
soil_frozen_water_content
Soil Frozen Water Content [CF-Standard Name]; unit: kg m-2
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
surface_upwelling_longwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_ice_surface_temperature
sea_ice_surface_temperature [CF-Standard Name]; unit: K
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_cloud_liquid_water_particles_in_air
number_concentration_of_cloud_liquid_water_particles_in_air [CF-Standard Name]; unit: m-3
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_black_carbon_dry_aerosol
Load of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-2
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
water_evaporation_flux_from_canopy
Evaporation from Canopy [CF-Standard Name]; unit: kg m-2 s-1
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
sea_ice_surface_temperature
sea_ice_surface_temperature [CF-Standard Name]; unit: K
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_eastward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
sea_surface_salinity
The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: psu
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
surface_downward_eastward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
mole_fraction_of_methane_in_air
Mole Fraction of CH4 [CF-Standard Name]; unit: 1e-9
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
leaf_area_index
"X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
sea_water_potential_temperature
sea_water_potential_temperature [CF-Standard Name]; unit: K
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
net_downward_radiative_flux_at_top_of_atmosphere_model
Net Downward Flux at Top of Model [CF-Standard Name]; unit: W m-2
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
sea_surface_salinity
The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: psu
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
relative_humidity
relative_humidity [CF-Standard Name]; unit: 0.01
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux_from_soil
Water means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called sublimation.) In accordance with common usage in geophysical disciplines, flux implies per unit area, called flux density in physics. [CF-Standard Name]; unit: kg m-2 s-1
effective_radius_of_stratiform_cloud_liquid_water_particles
Hydrometeor Effective Radius of Stratiform Cloud Liquid Water [CF-Standard Name]; unit: m
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
mole_fraction_of_nitrous_oxide_in_air
Mole Fraction of N2O [CF-Standard Name]; unit: 1e-9
atmosphere_mass_content_of_dust_dry_aerosol
Load of Dust [CF-Standard Name]; unit: kg m-2
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
atmosphere_mass_content_of_seasalt_dry_aerosol
Load of Seasalt [CF-Standard Name]; unit: kg m-2
water_evaporation_flux_from_canopy
Evaporation from Canopy [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
cell_thickness
Ocean Model Cell Thickness [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
net_downward_radiative_flux_at_top_of_atmosphere_model
Net Downward Flux at Top of Model [CF-Standard Name]; unit: W m-2
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
atmosphere_net_upward_convective_mass_flux
atmosphere_net_upward_convective_mass_flux [CF-Standard Name]; unit: kg m-2 s-1
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
lagrangian_tendency_of_air_pressure
"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_emission [CF-Standard Name]; unit: kg m-2 s-1
eastward_wind
"Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux_from_canopy
Evaporation from Canopy [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky
surface_upwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
surface_air_pressure
The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
toa_outgoing_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
sea_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
surface_snow_area_fraction
surface_snow_area_fraction [CF-Standard Name]; unit: 0.01
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
sea_ice_y_transport
sea_ice_y_transport [CF-Standard Name]; unit: kg s-1
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_water_vapor_content
"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. Atmosphere water vapor content is sometimes referred to as "precipitable water", although this term does not imply the water could all be precipitated.[CF-Standard Name]; unit: kg m-2
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
global_average_thermosteric_sea_level_change
Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
transpiration_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_of_carbon_dioxide
atmosphere_mass_of_carbon_dioxide [CF-Standard Name]; unit: kg
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_net_chemical_production_and_emission
[CF-Standard Name]; unit: kg m-2 s-1
water_evaporation_flux
"Water" means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called "sublimation".) In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
upward_ocean_mass_transport
Upward Ocean Mass Transport [CF-Standard Name]; unit: kg s-1
water_flux_into_sea_water_from_rivers
"Water" means water in all phases. The water flux or volume transport into sea water from rivers is the inflow to the ocean, often applied to the surface in ocean models. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
effective_radius_of_convective_cloud_liquid_water_particles
Convective Cloud Droplet Effective Radius [CF-Standard Name]; unit: m
temperature_in_surface_snow
temperature_in_surface_snow [CF-Standard Name]; unit: K
surface_downward_y_stress
surface_downward_y_stress [CF-Standard Name]; unit: N m-2
square_of_upward_ocean_mass_transport
Square of Upward Ocean Mass Transport [CF-Standard Name]; unit: kg2 s-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
surface_downward_eastward_stress
The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
toa_incoming_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation
tendency_of_sea_ice_amount_due_to_congelation_ice_accumulation [CF-Standard Name]; unit: kg m-2 s-1
heat_flux_into_sea_water_due_to_sea_ice_thermodynamics
Heat Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: W m-2
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
sea_ice_y_velocity
sea_ice_y_velocity [CF-Standard Name]; unit: m s-1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
water_evaporation_flux_from_soil
Water means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called sublimation.) In accordance with common usage in geophysical disciplines, flux implies per unit area, called flux density in physics. [CF-Standard Name]; unit: kg m-2 s-1
water_flux_into_sea_water
alias: water_flux_into_ocean
"Water" means water in all phases. The water flux into sea water is the freshwater entering as a result of precipitation, evaporation, river inflow, sea ice effects and water flux relaxation and correction (if applied). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
mole_fraction_of_ozone_in_air
Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: 1e-9
volume_extinction_coefficient_in_air_due_to_ambient_aerosol
[CF-Standard Name]; unit: m-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). 'Emission' is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
toa_incoming_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
northward_sea_water_velocity
sea_water_y_velocity [CF-Standard Name]; unit: m s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_due_to_dry_deposition
Dry Deposition Rate of SO4 [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "particulate_organic_matter_dry_aerosol" means all particulate organic matter dry aerosol except black carbon. It is the sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mass_fraction_of_cloud_liquid_water_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
toa_incoming_shortwave_flux
"shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
sea_water_mass_per_unit_area
Sea Water Mass Per Unit Area [CF-Standard Name]; unit: kg m-2
water_evaporation_flux_from_canopy
Evaporation from Canopy [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_temperature
Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice
heat_flux_into_sea_water_due_to_freezing_of_frazil_ice [CF-Standard Name]; unit: W m-2
atmosphere_number_content_of_cloud_droplets
Column Integrated Cloud Droplet Number [CF-Standard Name]; unit: m-2
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
toa_outgoing_longwave_flux
"longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
sea_water_mass
Sea Water Mass [CF-Standard Name]; unit: kg
air_pressure_at_convective_cloud_base
air_pressure_at_convective_cloud_base [CF-Standard Name]; unit: Pa
mass_concentration_of_dust_dry_aerosol_in_air
Concentration of Dust [CF-Standard Name]; unit: kg m-3
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads
tendency_of_sea_ice_amount_due_to_frazil_ice_accumulation_in_leads [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
rainfall_flux
rainfall_flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_sea_ice_amount_due_to_basal_melting
tendency_of_sea_ice_amount_due_to_basal_melting [CF-Standard Name]; unit: kg m-2 s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upwelling_shortwave_flux_in_air
The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
atmosphere_absorption_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Absorption Optical Thickness at 550 nm [CF-Standard Name]; unit: 1
surface_downwelling_longwave_flux_in_air
surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics
Virtual Salt Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
moisture_content_of_soil_layer
moisture_content_of_soil_layer [CF-Standard Name]; unit: kg m-2
surface_runoff_flux
The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
wind_speed
Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1
atmosphere_optical_thickness_due_to_ambient_aerosol
Ambient Aerosol Opitical Thickness at 550 nm [CF-Standard Name]; unit: 1
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
sea_ice_thickness
sea_ice_thickness [CF-Standard Name]; unit: m
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
tendency_of_sea_ice_amount_due_to_snow_conversion
[CF-Standard Name]; unit: kg m-2 s-1
atmosphere_mass_content_of_sulfate_dry_aerosol
Load of SO4 [CF-Standard Name]; unit: kg m-2
global_average_sea_level_change
Global Average Sea Level Change [CF-Standard Name]; unit: m
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_snow_amount
surface_snow_amount [CF-Standard Name]; unit: kg m-2
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
specific_humidity
"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
surface_upward_sensible_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_heat_flux_in_sea_water
surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2
sea_surface_temperature
Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: K
sea_ice_surface_temperature
sea_ice_surface_temperature [CF-Standard Name]; unit: K
tendency_of_atmosphere_mass_content_of_dimethyl_sulfide_due_to_dry_deposition
Dry Deposition Rate of DMS [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air
[CF-Standard Name]; unit: m-3
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
convective_precipitation_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
surface_downwelling_longwave_flux_in_air_assuming_clear_sky
surface_downwelling_longwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
mass_concentration_of_black_carbon_dry_aerosol_in_air
Surface Concentration of Black Carbon Aerosol [CF-Standard Name]; unit: kg m-3
mass_concentration_of_particulate_organic_matter_dry_aerosol_in_air
Concentration of Dry Aerosol Organic Matter [CF-Standard Name]; unit: kg m-3
cloud_area_fraction
"X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01
downward_sea_ice_basal_salt_flux
Downward Sea Ice Basal Salt Flux [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
sea_water_volume
Sea Water Volume [CF-Standard Name]; unit: m3
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_wet_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Wet deposition" means deposition by precipitation. [CF-Standard Name]; unit: kg m-2 s-1
surface_downward_x_stress
surface_downward_x_stress [CF-Standard Name]; unit: N m-2
effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top
effective_radius_of_cloud_liquid_water_particle_at_liquid_water_cloud_top [CF-Standard Name]; unit: m
number_concentration_of_cloud_liquid_water_particles_in_air
number_concentration_of_cloud_liquid_water_particles_in_air [CF-Standard Name]; unit: m-3
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
surface_downward_y_stress
surface_downward_y_stress [CF-Standard Name]; unit: N m-2
toa_outgoing_longwave_flux_assuming_clear_sky
A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2
runoff_flux
Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
surface_upward_latent_heat_flux
The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky
surface_downwelling_shortwave_flux_in_air_assuming_clear_sky [CF-Standard Name]; unit: W m-2
surface_downwelling_shortwave_flux_in_air
surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_sulfur_dioxide_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
surface_snow_thickness
surface_snow_thickness [CF-Standard Name]; unit: m
tendency_of_sea_ice_amount_due_to_lateral_growth_of_ice_floes
Lateral Sea Ice Growth Rate
Used in MIP table(s): CMOR Table OImon: Monthly Mean Ocean Cryosphere Fields
Comment in standard_output document: the rate of change of sea ice mass due to lateral growth alone of the sea ice divided by the area of the ocean portion of the grid cell. Reported as 0.0 in regions free of sea ice.
Code list created on 2012-10-16 out of standard_output document (http://cmip-pcmdi.llnl.gov/cmip5/docs/standard_output.xlsx )
cf:"Amount" means mass per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "tendency_of_X" means derivative of X with respect to time. An ice floe is a flat expanse of sea ice, generally taken to be less than 10 km across. "Lateral growth of ice floe" means the accumulation of ice at the extreme edges of the ice area. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_sulfate_expressed_as_sulfur_dry_aerosol_due_to_wet_deposition
[CF-Standard Name]; unit: kg m-2 s-1
snowfall_flux
In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1
tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_due_to_dry_deposition
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. "Dry deposition" means gravitational settling, impact scavenging and turbulent deposition. [CF-Standard Name]; unit: kg m-2 s-1
mass_concentration_of_sulfate_dry_aerosol_in_air
Concentration of SO4 [CF-Standard Name]; unit: kg m-3
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top
number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top [CF-Standard Name]; unit: m-3
air_pressure_at_convective_cloud_top
air_pressure_at_convective_cloud_top [CF-Standard Name]; unit: Pa
tendency_of_atmosphere_mass_content_of_black_carbon_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. earth's surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
northward_wind
"Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1
air_pressure_at_sea_level
sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: Pa
geopotential_height
Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m
surface_snow_melt_flux
The surface called "surface" means the lower boundary of the atmosphere. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. For unit "m day-1" the water equivalent of snow melt is given. [CF-Standard Name]; unit: kg m-2 s-1
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top
number_concentration_of_ice_crystals_in_air_at_ice_cloud_top [CF-Standard Name]; unit: m-3
mass_concentration_of_seasalt_dry_aerosol_in_air
Surface Concentration of Seasalt [CF-Standard Name]; unit: kg m-3
mass_fraction_of_cloud_ice_in_air
Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: 1
sea_water_salinity
sea_water_salinity [CF-Standard Name]; unit: psu
water_flux_into_sea_water_due_to_sea_ice_thermodynamics
Water Flux into Sea Water due to Sea Ice Thermodynamics [CF-Standard Name]; unit: kg m-2 s-1
area_fraction
"Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01
cloud_area_fraction_in_atmosphere_layer
"Layer" means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. "X_area_fraction" means the fraction ofhorizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". [CF-Standard Name]; unit: 0.01
tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_due_to_emission
"tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol" means aerosol without water. located anywhere within the atmosphere, including at the lower boundary (i.e. earth' surface). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. [CF-Standard Name]; unit: kg m-2 s-1
surface_temperature
The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K
net_downward_radiative_flux_at_top_of_atmosphere_model
Net Downward Flux at Top of Model [CF-Standard Name]; unit: W m-2
NetCDF
53639758
https://www.wdc-climate.de/ui/entry?acronym=MIM5DEC
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EBAS.LV0010R.20140101080000.20170510114239.mass_concentration_of_sulfate_dry_aerosol_particles_in_air.aerosol.1d.2
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https://sru.dwd.de/SRU2JDBC/