1.1
3013
1541611395
info:srw/schema/1/example-v1.1
xml:ISO19139:F
de.dwd.mosmix.14544
eng
utf8
dataset
Kai-Thorsten Wirt
Deutscher Wetterdienst
RTH FOCAL POINT
+49 (0) 69 8062-2546
Frankfurter Straße 135
Offenbach
63067
Germany
gisc@dwd.de
http://www.dwd.de
pointOfContact
2018-04-25T00:00:00Z
WMO Core Metadata Profile of ISO 19115 (WMO Core), 2003/Cor.1:2006 (ISO 19115), 2007 (ISO/TS 19139)
1.3
WGS 84
World Geodetic System
http://www.wmo.int/pages/prog/wis/2012/metadata/version_1-3/
WMO Core Profile version 1.3
Model Output Statistics for BUGOJNO (14544)
2018-04-25
creation
2018-04-25
publication
2018-04-25
revision
de.dwd.mosmix.14544
http://wis.wmo.int
Kai-Thorsten Wirt
Deutscher Wetterdienst
RTH FOCAL POINT
+49 (0) 69 8062-2546
Frankfurter Straße 135
Offenbach
63067
Germany
gisc@dwd.de
http://www.dwd.de
distributor
documentDigital
The dot notation recommended by WMO-CBS IPET-MDRD is used to build the code identifier
DWD’s fully automatic MOSMIX product optimizes and interprets the forecast calculations of the NWP models ICON (DWD) and IFS (ECMWF), combines these and calculates statistically optimized weather forecasts in terms of point forecasts (PFCs). Thus, statistically corrected, updated forecasts for the next ten days are calculated for about 5400 locations around the world. Most forecasting locations are spread over Germany and Europe. MOSMIX forecasts (PFCs) include nearly all common meteorological parameters measured by weather stations.
For further information please refer to:
[in German: https://www.dwd.de/DE/leistungen/met_verfahren_mosmix/met_verfahren_mosmix.html ]
[in English: https://www.dwd.de/EN/ourservices/met_application_mosmix/met_application_mosmix.html ]
NC/DCPC
Kai-Thorsten Wirt
Deutscher Wetterdienst
Focal Point
T+49 69 8062 2546
Frankfurter Straße 135
OFFENBACH
63067
Germany
gisc@dwd.de
originator
continual
dataset
The details of the update frequence are described in the temporalElement
03
09
15
21
temporal
Dewpoint
Forecast
MOS
Maximum Temperature
Minimum Temperature
Model Output Statistics
Past weather
Precipitation
Present weather
Temperature
Total cloud cover
Visibility
Wind
Wind gust
theme
meteorology
theme
WMO_CategoryCode
2012-06-27
revision
Codelists for description of metadata datasets compliant with the WMO Core
Metadata Profile version 1.3 [http://wis.wmo.int/2013/codelists/WMOCodeLists.xml]
2012-06-27
revision
WMO_CategoryCode
WMO Secretariat
publisher
14544
BUGOJNO
Bosnia and Herzegowina
place
Meteorological geographical features
GEMET - INSPIRE themes, version
1.0
2008-06-01
publication
Dewpoint
Forecast
Maximum Temperature
Minimum Temperature
Past weather
Precipitation
Present weather
Temperature
Visibility
Wind
Wind gust
cloud cover
dataParam
WMOEssential
otherRestrictions
otherRestrictions
WMOEssential
eng
utf8
climatologyMeteorologyAtmosphere
The product/data covers the following region/bounding box: south=44.025, north=44.115, west=17.425, east=17.515
17.425
17.515
44.025
44.115
2018-04-25Z
: Model Output Statistics for BUGOJNO (14544)
thematicClassification
kmz
http://www.wmo.int/pages/prog/www/WMOCodes.html
https://gisc.dwd.de/angular-frontend/xmlProductDetails;pid=de.dwd.mosmix.14544
http
GISC Offenbach, Deutscher Wetterdienst
WMO Information System, download products/data through GISC Offenbach, Deutscher Wetterdienst
dataset
INSPIRE Data Specification on Meteorological geographical features
2010-12-08
publication
See the referenced specification
true
High data quality controlled according to the procedures of the WIS
This metadata record was created automatically as a representation of the bulletin
declaration found in WMO # 9 Volume C1. Other references were used in the process, including WMO
References such as WMO # 9 Volume A, WMO # 386 Manual on the GTS and WMO # 306 Manual on Codes. Other
elements of information were also collected or created for the purpose of the GTS Metadata Generation.
This work, as well as the creation of the representation of the WMO references was done by Deutscher
Wetterdienst (DWD) on a "best effort" basis.
]]>
1
info:srw/schema/1/example-v1.1
xml:ISO19139:F
wdc-climate.de:3607581
eng; USA
collection
BNSClim_hydro_v1.0
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
pointOfContact
2018-05-25T08:59:23
ISO 19115
ISO 19115-2:2009
Baltic and North Sea Climatology hydrographic part (Version 1.0)
2018-11-21
publication
1
BNSClim_hydro_v1.0
doi:10.1594/WDCC/BNSClim_hydro_v1.0
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
Email: iris.hinrichs@uni-hamburg.de
originator
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
Email: iris.hinrichs@uni-hamburg.de
author
Dr. Viktor Gouretski
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
Email: viktor.gouretski@uni-hamburg.de
author
WDC Climate at DKRZ
publisher
This is the first version (v1.0) of the hydrographic part of the "Baltic and North Sea Climatology (BNSC)". The parameters provided here are water temperature and salinity on 105 depth levels. The data product comprises the time period from 1873-2015 and is based on more than one million observational profiles, which were obtained from several different data sources in the region of the Baltic, the North Sea and adjacent areas of the North Atlantic Ocean (15°W-30°E, 47°N-66°N). Intersection of observational data from different data sources is avoided and the in situ data were objected to an elaborate automatic quality control to identify erroneous observations that would bias the data product. Additionally, a correction of the temporal sampling error was applied to minimize the impact of the temporal distribution of the observations on the created temporal mean fields.
The data product consists of gridded mean fields of water temperature and salinity. The spatial resolution is 0.25° in meridional and zonal direction. The depth levels are irregularly distributed: for the depth interval from 0 to 50m the distance between the single depth levels is 5m. Below 50m, the distance increases progressively by 1m to the last depth level of 4985m. The dimensions of the data product are 180*76*105 (longitude, latitude, depth). The BNSC climatology consists, on the one hand, of time series of monthly and annual mean values of the hydrographic parameters as fields of box averages. Grid boxes that show no observations are left empty. Based on these time series, decadal monthly mean fields are created for the decades 1956-1965, 1966-1975, 1976-1985, 1986-1995, 1996-2005, 2006-2015 as another part of the data product. Again, gaps remain in observational data-void regions.
The third part of the data product results from above mentioned decadal mean fields: horizontally interpolated fields by application of the method of objective analysis. Consequently, this subset does not contain gaps.
Available parameters:
box averages: monthly and annual mean, resp. standard deviation, number of observations
decadal box averages: decadal monthly mean, resp. standard deviation, mean year, standard deviation to mean year, number of years
decadal interpolated mean: interpolated monthly mean, absolute median deviation, number of bins, first guess, relative interpolation error, mean year, mean distance
The products are publicly available at the ICDC portal ( https://icdc.cen.uni-hamburg.de/1/daten/ocean/bnsc/)
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
pointOfContact
NetCDF
In Situ Ocean-based Platforms
Temperature/Humidity Sensors
CC BY 4.0: Creative Commons Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/
eng; USA
-15.0
30.0
47.0
66.0
calendrical
1873-01-01
2015-12-31
land_binary_mask
X_binary_mask has 1 where condition X is met, 0 elsewhere. 1 = land, 0 = sea. [CF-Standard Name]; unit: 1
land_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.[CF-Standard Name]; unit: 1
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
NetCDF
62531
https://www.wdc-climate.de/ui/entry?acronym=BNSClim_hydro_v1.0
information
collection
n/a
None
]]>
2
info:srw/schema/1/example-v1.1
xml:ISO19139:F
wdc-climate.de:3850389
eng; USA
collection
BNSClimHydrov1.1
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
pointOfContact
Remon Sadikni
University of Hamburg / ICDC
http://icdc.zmaw.de
pointOfContact
2019-05-28T11:14:28
ISO 19115
ISO 19115-2:2009
Baltic and North Sea Climatology hydrographic part (Version 1.1). World Data Center for Climate (WDCC) at DKRZ.
2019-09-16
publication
1
BNSClimHydrov1.1
doi:10.26050/WDCC/BNSClimHydrov1.1
Remon Sadikni
University of Hamburg / ICDC
http://icdc.zmaw.de
Email: remon.sadikni@uni-hamburg.de
principalInvestigator
Dr. Iris Hinrichs
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
Email: iris.hinrichs@uni-hamburg.de
author
Dr. Viktor Gouretski
Center for Earth System Research and Sustainability, University of Hamburg
http://www.cen.uni-hamburg.de/
Email: viktor.gouretski@uni-hamburg.de
author
WDC Climate at DKRZ
publisher
This is version v1.1 of the hydrographic part of the "Baltic and North Sea Climatology (BNSC)".
It turned out that the original hydrographic data product of the BNSC
(BNSClim hydrographic part (Version 1.0)) was erroneous. The errors occurred by accidentally reading obsolete files in two of the intermediate steps of the production procedure. By this, the basis of observations was altered. This happened after the quality control and interpolation of the observations on standard depths, in the step where the observations are sorted into the chosen grid (this affects temperature and salinity) and in the following step, the correction of the temporal sampling error (this affects only salinity).
These errors were corrected in this Version 1.1.
The parameters provided are water temperature and salinity on 105 depth levels. The data product comprises the time period from 1873-2015 and is based on more than one million observational profiles, which were obtained from several different data sources in the region of the Baltic, the North Sea and adjacent areas of the North Atlantic Ocean (15°W-30°E, 47°N-66°N). Intersection of observational data from different data sources is avoided and the in situ data were objected to an elaborate automatic quality control to identify erroneous observations that would bias the data product. Additionally, a correction of the temporal sampling error was applied to minimize the impact of the temporal distribution of the observations on the created temporal mean fields.
The data product consists of gridded mean fields of water temperature and salinity. The spatial resolution is 0.25° in meridional and zonal direction. The depth levels are irregularly distributed: for the depth interval from 0 to 50m the distance between the single depth levels is 5m. Below 50m, the distance increases progressively by 1m to the last depth level of 4985m. The dimensions of the data product are 180*76*105 (longitude, latitude, depth). The BNSC climatology consists, on the one hand, of time series of monthly and annual mean values of the hydrographic parameters as fields of box averages. Grid boxes that show no observations are left empty. Based on these time series, decadal monthly mean fields are created for the decades 1956-1965, 1966-1975, 1976-1985, 1986-1995, 1996-2005, 2006-2015 as another part of the data product. Again, gaps remain in observational data-void regions.
The third part of the data product results from above mentioned decadal mean fields: horizontally interpolated fields by application of the method of objective analysis. Consequently, this subset does not contain gaps.
Available parameters:
box averages: monthly and annual mean, resp. standard deviation, number of observations
decadal box averages: decadal monthly mean, resp. standard deviation, mean year, standard deviation to mean year, number of years
decadal interpolated mean: interpolated monthly mean, absolute median deviation, number of bins, first guess, relative interpolation error, mean year, mean distance
The products and a description of the differences between v1.0 and v1.1 are publicly available at the ICDC portal ( https://icdc.cen.uni-hamburg.de/1/daten/ocean/bnsc/)
Remon Sadikni
University of Hamburg / ICDC
http://icdc.zmaw.de
pointOfContact
NetCDF
In Situ Ocean-based Platforms
Temperature/Humidity Sensors
data assimilation
CC BY 4.0: Creative Commons Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/
eng; USA
-15.0
30.0
47.0
66.0
calendrical
1873-01-01
2015-12-31
land_binary_mask
X_binary_mask has 1 where condition X is met, 0 elsewhere. 1 = land, 0 = sea. [CF-Standard Name]; unit: 1
land_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.[CF-Standard Name]; unit: 1
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_practical_salinity
cf:Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448. [CF-Standard Name]; unit: 1
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
sea_water_temperature
Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990. [CF-Standard Name]; unit: degC
NetCDF
62532
https://www.wdc-climate.de/ui/entry?acronym=BNSClimHydrov1.1
information
collection
n/a
None
]]>
3
info:srw/schema/1/example-v1.1
xml:ISO19139:F
urn:x-wmo:md:int.wmo.wis::SIQB40LQSM
eng
utf8
dataset
Series of WMO GTS Bulletins;
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
pointOfContact
2016-03-29T07:14:35Z
WMO Core Metadata Profile of ISO 19115 (WMO Core), 2003/Cor.1:2006 (ISO 19115), 2007 (ISO/TS 19139)
1.3
WGS 84
World Geodetic System
http://www.wmo.int/pages/prog/wis/2012/metadata/version_1-3/
WMO Core Profile version 1.3
GTS Bulletin: SIQB40 LQSM - Surface data (details are described in the abstract)
2014-09-22Z
publication
2016-03-29Z
revision
urn:x-wmo:md:int.wmo.wis::SIQB40LQSM
http://wis.wmo.int
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
distributor
documentDigital
The dot notation recommended by WMO-CBS IPET-MDRD is used to build the code identifier
The SIQB40 TTAAii Data Designators decode as: T1 (S): Surface data T1T2 (SI): Intermediate synoptic hour A1A2 (QB): Bosnia and Herzegovina(The bulletin collects reports from stations: 14557;TUZLA / BOSNIA;14640;LIVNO / BOSNIA;14528;BIHAC (13228);14537;SANSKI MOST;14544;BUGOJNO;) (Remarks from Volume-C: XXX)
WMO GTS Bulletin - Intended for global Exchange
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
originator
continual
dataset
The details of the update frequence are described in the temporalElement
09
15
temporal
Intermediate synoptic hour
SYNOP
cloud
cover
dewpoint
duration
gust
humidity
maximum
minimum
precipitation
pressure
radiation
snow
soil
solar
speed
surface
temperature
visibility
weather
wind
theme
meteorology
synopticMeteorology
weatherObservations
theme
WMO_CategoryCode
2012-06-27
revision
Codelists for description of metadata datasets compliant with the WMO Core
Metadata Profile version 1.3 [http://wis.wmo.int/2013/codelists/WMOCodeLists.xml]
2012-06-27
revision
WMO_CategoryCode
WMO Secretariat
publisher
14528
14537
14544
14557
14640
BIHAC (13228)
BUGOJNO
Bosnia and Herzegovina
LIVNO / BOSNIA
SANSKI MOST
TUZLA / BOSNIA
place
Meteorological geographical features
GEMET - INSPIRE themes, version
1.0
2008-06-01
publication
GlobalExchange
dataCentre
WMO_DistributionScopeCode
2012-06-27
revision
WMOAdditional
otherRestrictions
otherRestrictions
WMOAdditional
GTSPriority2
eng
utf8
climatologyMeteorologyAtmosphere
The product/data covers the following region/bounding box: Bosnia and Herzegovina
15.74059
19.61979
42.56583
45.26595
2014-09-22Z
SIQB40 : GTS Bulletin: SIQB40 LQSM - Surface data (details are described in the abstract)
thematicClassification
FM 12
-
http://www.wmo.int/pages/prog/www/WMOCodes.html
https://gisc.dwd.de/angular-frontend/xmlProductDetails;pid=urn:x-wmo:md:int.wmo.wis::SIQB40LQSM
http
GISC Offenbach, Deutscher Wetterdienst
WMO Information System, download products/data through GISC Offenbach, Deutscher Wetterdienst
dataset
INSPIRE Data Specification on Meteorological geographical features
2010-12-08
publication
See the referenced specification
true
High data quality controlled according to the procedures of the WIS
This metadata record was created automatically as a representation of the bulletin
declaration found in WMO # 9 Volume C1. Other references were used in the process, including WMO
References such as WMO # 9 Volume A, WMO # 386 Manual on the GTS and WMO # 306 Manual on Codes. Other
elements of information were also collected or created for the purpose of the GTS Metadata Generation.
This work, as well as the creation of the representation of the WMO references was done by Deutscher
Wetterdienst (DWD) on a "best effort" basis.
]]>
4
info:srw/schema/1/example-v1.1
xml:ISO19139:F
urn:x-wmo:md:int.wmo.wis::ISID02LQSM
eng
utf8
dataset
Series of WMO GTS Bulletins;
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
pointOfContact
2021-05-20T10:58:49Z
WMO Core Metadata Profile of ISO 19115 (WMO Core), 2003/Cor.1:2006 (ISO 19115), 2007 (ISO/TS 19139)
1.3
WGS 84
World Geodetic System
http://www.wmo.int/pages/prog/wis/2012/metadata/version_1-3/
WMO Core Profile version 1.3
GTS Bulletin: ISID02 LQSM - Observational data (Binary coded) - BUFR (details are described in the abstract)
2012-02-01Z
creation
2012-02-01Z
publication
2021-05-20Z
revision
urn:x-wmo:md:int.wmo.wis::ISID02LQSM
http://wis.wmo.int
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
distributor
documentDigital
The dot notation recommended by WMO-CBS IPET-MDRD is used to build the code identifier
The ISID02 TTAAii Data Designators decode as: T1 (I): Observational data (Binary coded) - BUFR T1T2 (IS): Surface/sea level T1T2A1 (ISI): Intermediate synoptic observations from fixed land stations A2 (D): 90°E - 0° northern hemisphere(The bulletin collects reports from stations: 14528;BIHAC (13228);14537;SANSKI MOST;14543;JAJCE;14544;BUGOJNO;14549;ZENICA / BOSNIA;14554;GRADACAC;14557;TUZLA / BOSNIA;14640;LIVNO / BOSNIA;14650;IVAN SEDLO;14657;NEUM;) (Remarks from Volume-C: XXX)
WMO GTS Bulletin - Intended for global Exchange
NMC BOSNIA AND HERZEGOVINA - Federal Hydrometorological Institute
T+387 033276700
F+387 033276701
Bardakcije 12
SARAJEVO
71000
Bosnia and Herzegovina
contact@fhmzbih.gov.ba
originator
continual
dataset
The details of the update frequence are described in the temporalElement
03
09
15
21
temporal
Binary universal form for the representation of meteorological data
SYNOP
cloud
cover
dewpoint
duration
gust
humidity
maximum
minimum
precipitation
pressure
radiation
snow
soil
solar
speed
surface
temperature
visibility
weather
wind
theme
meteorology
synopticMeteorology
weatherObservations
theme
WMO_CategoryCode
2012-06-27
revision
Codelists for description of metadata datasets compliant with the WMO Core
Metadata Profile version 1.3 [http://wis.wmo.int/2013/codelists/WMOCodeLists.xml]
2012-06-27
revision
WMO_CategoryCode
WMO Secretariat
publisher
14528
14537
14543
14544
14549
14554
14557
14640
14650
14657
BIHAC (13228)
BUGOJNO
GRADACAC
IVAN SEDLO
JAJCE
LIVNO / BOSNIA
NEUM
SANSKI MOST
TUZLA / BOSNIA
ZENICA / BOSNIA
place
Meteorological geographical features
GEMET - INSPIRE themes, version
1.0
2008-06-01
publication
GlobalExchange
dataCentre
WMO_DistributionScopeCode
2012-06-27
revision
WMOAdditional
otherRestrictions
otherRestrictions
WMOAdditional
GTSPriority2
eng
utf8
climatologyMeteorologyAtmosphere
The product/data covers the following region/bounding box: 90°E - 0° northern hemisphere
15.8833
18.7
42.9167
44.8833
2012-02-01Z
ISID02 : GTS Bulletin: ISID02 LQSM - Observational data (Binary coded) - BUFR (details are described in the abstract)
thematicClassification
FM 94
http://www.wmo.int/pages/prog/www/WMOCodes.html
https://gisc.dwd.de/angular-frontend/xmlProductDetails;pid=urn:x-wmo:md:int.wmo.wis::ISID02LQSM
http
GISC Offenbach, Deutscher Wetterdienst
WMO Information System, download products/data through GISC Offenbach, Deutscher Wetterdienst
dataset
INSPIRE Data Specification on Meteorological geographical features
2010-12-08
publication
See the referenced specification
true
High data quality controlled according to the procedures of the WIS
This metadata record was created automatically as a representation of the bulletin
declaration found in WMO # 9 Volume C1. Other references were used in the process, including WMO
References such as WMO # 9 Volume A, WMO # 386 Manual on the GTS and WMO # 306 Manual on Codes. Other
elements of information were also collected or created for the purpose of the GTS Metadata Generation.
This work, as well as the creation of the representation of the WMO references was done by Deutscher
Wetterdienst (DWD) on a "best effort" basis.
]]>
5
6
1.1
de.dwd.mosmix.14544
1
5
xml
https://sru.dwd.de/SRU2JDBC/