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xml:ISO19139:F
de.dkrz.wdcc.iso3889342
series
RRA_WRF_simulations
Xun Wang
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Benjamin Schmidt
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Prof. Dr. Dieter Scherer
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Dr. Marco Otto
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Dr. Marco Otto
Technische Universität Berlin
https://www.klima.tu-berlin.de/
pointOfContact
Prof. Dr. Dieter Scherer
Technische Universität Berlin
https://www.klima.tu-berlin.de/
originator
2021-07-14T04:25:20
ISO 19115
ISO 19139 / DKRZ ISO Simple Profile V1.0
http://doi.org/doi:10.26050/WDCC/RRA_WRF_simulations
RRA WRF simulations of the mid-Pliocene and present-day conditions over High Mountain Asia
RRA WRF simulations of the mid-Pliocene and present-day conditions over High Mountain Asia
2021-06-28
creation
None
WRF dynamical downscaling of present-day and mid-Pliocene atmospheric conditions over High Mountain Asia
doi:10.26050/WDCC/RRA_WRF_simulations
Prof. Dr. Dieter Scherer
Technische Universität Berlin
https://www.klima.tu-berlin.de/
originator
doi:10.26050/WDCC/RRA_WRF_simulations
The data was produced employing the Advanced Research Weather Research and Forecasting model (WRF) version 4.1.2 (Skamarock et al., 2019) for the dynamical downscaling of GCM data. WRF is a fully compressible non-hydrostatic atmospheric simulation system. Two sensitivity simulations were conducted using 15-year time slices for the present day and the mid-Pliocene simulated by ECHAM5 as initial and boundary conditions (Mutz et al., 2018; Botsyun et al., 2020). Except for the atmospheric forcing data, other parameters were the same in both simulations.
The model domain has a grid spacing of 30 km. In the vertical direction, 28 terrain-following eta-levels were used. The model time steps are 120 seconds with a 6 hourly data output and are aggregated to daily values in post processing. The boundary conditions were updated every 6 h. The daily re-initialization strategy from Maussion et al. (2011) and Maussion et al. (2014) were employed: each simulation starts at 12 UTC and contains 36 h, with the first 12 h as the spin-up time. This strategy kept the large-scale circulation patterns simulated by WRF closely constrained by the forcing data, while concurrently allowing WRF to develop the mesoscale atmospheric features. Physical parameterization schemes were consistent with the ones used for high-resolution dynamical downscaling in High Mountain Asia in Wang et al. (2021). The data format follows the guidelines of the [UC]² Data Standard (http://www.uc2-program.org/uc2_data_standard.pdf).
Xun Wang
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Benjamin Schmidt
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Prof. Dr. Dieter Scherer
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Dr. Marco Otto
Technische Universität Berlin
https://www.klima.tu-berlin.de/
author
Dr. Marco Otto
Technische Universität Berlin
https://www.klima.tu-berlin.de/
pointOfContact
WRF
theme
model data
theme
dynamical downscaling
theme
refined analysis
theme
regional climate modeling
theme
eng
23.6333
142.3667
-0.8014
60.1141
1903-01-01
1917-12-31
15
2000-01-01
2014-12-31
15
NetCDF
network Common Data Format
distributor
http://doi.org/doi:10.26050/WDCC/RRA_WRF_simulations
series
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