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DOI for Scientific and Technical Data
10.1594/WDCC/CLM_A1B_1_D3

URN
urn:nbn:de:tib-10.1594/WDCC/CLM_A1B_1_D33
Title
Climate Simulation with CLM, Scenario A1B run no.1, Data Stream 3: European region MPI-M/MaD
Citation
Lautenschlager,Michael; Keuler,Klaus; Wunram,Claudia; Keup-Thiel,Elke; Schubert, Martina; Will,Andreas; Rockel,Burkhardt; Boehm,Uwe 2009; Climate Simulation with CLM, Scenario A1B run no.1, Data Stream 3: European region MPI-M/MaD. World Data Center for Climate. [doi: 10.1594/WDCC/CLM_A1B_1_D3]
Publication Date
2009-04-02
Author(s)
Lautenschlager,Michael; Keuler,Klaus; Wunram,Claudia; Keup-Thiel,Elke; Schubert, Martina; Will,Andreas; Rockel,Burkhardt; Boehm,Uwe
Summary
The experiment CLM_A1B_1_D3 contains European regional climate simulations of the years 2001-2100 on a regular geographical grid. The data are generated during post processing of the corresponding data stream 2 experiment (CLM_A1B_1_D2) of regional climate model runs (CLM non hydrostatic, see http://clm.gkss.de ). It is forced by the first (_1_) run of the global IPCC scenario A1B (EH5-T63L31_OM-GR1.5L40_A1B_1_6H), which describes a possible future world of very rapid economic growth, global population peaking in mid-century and rapid introduction of new and more efficient technologies with a balance across all energy sources.
In data stream 3 (_D3) the output variables of CLM data stream 2 and some additionally derived parameters are stored as time series on a regular geograhical grid (0.2 deg. hor. res.). The transformation has been done via CDO routines. Please note, that none of the variables has been corrected for topographical differences between the two grids.
The model domain of data stream 3 covers the European region starting at 34.6/-10.6 (lat/lon, centre of lower left grid box) with an increment of 0.2 degree. The number of grid points is 177/238 (lat/lon).
For some model variables and additionally derived parameters some statistics on daily, monthly or yearly basis are available. See also http://sga.wdc-climate.de for a list of available parameters.
Please contact sga"at"dkrz.de for data request details.
See http://sga.wdc-climate.de for more details on CLM simulations in the context of the BMBF funding priority "klimazwei", some useful information on handling climate model data and the data access regulations.
The output format is netCDF
Experiment with CLM 2.4.11 on NEC-SX6(hurrikan)
raw data: archive.dkrz.de:/ut/k/k204095/prism/experiments/A1B_1
Location(s)
Europe; Latitude: 34.809 to 80.764; Longitude: -31.29 to 66.427
Spatial Coverage
Latitude: 34.6 to 69.8; Longitude: -10.6 to 36.8; Altitude: -3.82 m to 200.0 hPa
Temporal Coverage
1/1/2001 - 31/12/2100 (calendrical)
Data Format(s)
netCDF
Datasize
5565217228144 Bytes
Contact
Dr. Michael Lautenschlager
Max-Planck-Institut fuer Meteorologie
Model and Data
Beim Schlump 58, 20144 Hamburg, Germany
http://www.mad.zmaw.de/
Project
CLM regional climate model runs forced by the global IPCC scenario runs (CLM_regional_climate_model_runs)
These regional climate simulations have been funded by the BMBF and computed at DKRZ by the group "Model and Data" of MPI-M, Hamburg, in close cooperation with BTU Cottbus, GKSS Geesthacht and PIK Potsdam. Serving as community model, the climate version of the local model (CLM) of the DWD was used to simulate the regional climate of the 20th century (1960-2000) and 21st century (2001-2100) in Europe. The regional model runs are forced by the global IPCC scenario runs (http://www.grida.no/climate/ipcc/emission/index.htm ) to explore future developments in the European climate on a regional scale.
CLM (see http://clm.gkss.de ) was run in non hydrostatic mode with 0.165 degree horizontal grid resolution and was forced 6 hourly by the output of the global climate model runs with ECHAM5/MPIOM. The climate of the 20th century was simulated by three 20th century realization runs, set off at different initialization times. The climate of the 21st century was modeled with respect to two IPCC-climate scenarios (A1B and B1) with different assumptions regarding the development of global greenhouse gas concentrations.
For storage in and download from this data base, the data has been transformed into time series of single model variables and is provided in two different data streams (referenced as "data stream 2" and "data stream 3"). Data stream 2 is given on a rotated grid with 0.165 deg. spatial resolution (rotated coordinates). Data stream 3 is projected onto a non-rotated grid with 0.2 deg. spatial resolution (usual geographical coordinates). For the data transformation between the respective grids the cdo-routines have been used.
For the original model output (referenced as "data stream 0" and "data stream 1") please contact model(at)dkrz.de for further information.
See http://sga.wdc-climate.de for more details on CLM simulations in the context of the BMBF funding priority "klimazwei", some useful information on handling climate model data and the data access regulations.
Supplementary info
More information for this CERA experiment is available here.
Available Datasets (374)
<< Prev 25    [Page 1 of 15]    Next 25 >>

  Name Progress
CLM_A1B_1_D3_d_GZ0: surface_roughness_length (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_HMO3: air_pressure_at_ozone_maximum (D3 via bilinear interpolation) complete
CLM_A1B_1_D3_d_HZEROCL: freezing_level_altitude (D3 via bilinear interpolation) complete
CLM_A1B_1_D3_d_LAI: leaf_area_index (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_PLCOV: vegetation_area_fraction (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_ROOTDP: root_depth (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_SNOWLMT: snowfall_limit_altitude (D3 via bilinear interpolation) complete
CLM_A1B_1_D3_d_T_SNOW: surface_temperature_where_snow (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0001: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0004: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0010: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0022: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0046: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0094: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0190: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_T_SO_0382: soil_temperature (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_VIO3: equivalent_pressure_of_atmosphere_ozone_content (D3 via bilinear interpolation) complete
CLM_A1B_1_D3_d_W_I: canopy_water_amount (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0001: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0004: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0010: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0022: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0046: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0094: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete
CLM_A1B_1_D3_d_W_ICE_0190: lwe_thickness_of_frozen_water_content_of_soil_layer (D3 via nearest neighbour method) complete


Please note: