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, HZG Geesthacht and PIK Potsdam.
The experiment CLM_C20_3_D2 contains European regional climate simulations of the years 1960-2000 on a rotated grid (CLM non hydrostatic, 0.165 degree hor. resolution, see http://www.clm-community.eu ).
The experiment CLM_C20_3_D3 contains European regional climate simulations of the years 1960-2000 on a regular geographical grid. The data are generated during post processing of the corresponding data
The experiment CLM_C20_2_D2 contains European regional climate simulations of the years 1960-2000 on a rotated grid (CLM non hydrostatic, 0.165 degree hor. resolution, see http://www.clm-community.eu ).
The experiment CLM_C20_2_D3 contains European regional climate simulations of the years 1960-2000 on a regular geographical grid. The data are generated during post processing of the corresponding data
The experiment CLM_A1B_2_D2 contains European regional climate simulations of the years 2001-2100 on a rotated grid (CLM non hydrostatic, 0.165 deg. hor. resolution, see http://www.clm-community.eu ).
The experiment CLM_A1B_2_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
The experiment CLM_B1_2_D2 contains European regional climate simulations of the years 2001-2100 on a rotated grid (CLM non hydrostatic, 0.165 deg. hor. res., see http://www.clm-community.eu ). It is forced
The experiment CLM_B1_2_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
The experiment CLM_A1B_1_D2 contains European regional climate simulations of the years 2001-2100 on a rotated grid (CLM non hydrostatic, 0.165 deg. hor. resolution, see http://www.clm-community.eu ).
The experiment CLM_C20_1_D3 contains European regional climate simulations of the years 1960-2000 on a regular geographical grid. The data are generated during post processing of the corresponding data
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
The experiment CLM_C20_1_D2 contains European regional climate simulations of the years 1960-2000 on a rotated grid (CLM non hydrostatic, 0.165 degree hor. resolution, see http://www.clm-community.eu ).
The experiment CLM_B1_1_D2 contains European regional climate simulations of the years 2001-2100 on a rotated grid (CLM non hydrostatic, 0.165 deg. hor. res., see http://www.clm-community.eu ). It is forced
The experiment CLM_B1_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
The experiment CLM_C20_2_D3 contains European regional climate simulations of the years 1960-2000 on a regular geographical grid. The data are generated during post processing of the corresponding data
Plots include the following comparisons: Comparison_1: observations and CLM/ERA40 Comparison_2: CLM/ERA40 and CLM/20C3M (20C3M : 20th century IPCC AR4) Comparison_3: CLM/20C3M and ECHAM5/20C3M Comparison_4:
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is bilinear interpolation (cdo genbil, cdo remap).-- exp.summary: The experiment CLM_C20_2_D3 contains
This pdf file contains general information on the CERA database project 'CLM_regional_climate_model_runs', important user information, including a part on 'rights of use' and special information about some single parameter.
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is bilinear interpolation (cdo genbil, cdo remap). Please note that this parameter is provided for both
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is nearest neighbour method (cdo remapdis1). Please note that this parameter is provided for both transformation
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is bilinear interpolation (cdo genbil, cdo remap). Please note that this parameter is provided for both
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is nearest neighbour method (cdo remapdis1). Please note that this parameter is provided for both transformation
Describes the dominating soil type of the land fraction in the grid cell according to the following classes: 1: ice, 2: rock, 3: sand, 4:sandy loam, 5: loam, 6: loamy clay, 7: clay, 8: peat, 9: water.
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is bilinear interpolation (cdo genbil, cdo remap). Please note that this parameter is provided for both
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is nearest neighbour method (cdo remapdis1). Please note that this parameter is provided for both transformation
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is bilinear interpolation (cdo genbil, cdo remap). Please note that this parameter is provided for both
For this parameter the transformation procedure from the rotated grid (D2) to the regular grid (D3) is nearest neighbour method (cdo remapdis1). Please note that this parameter is provided for both transformation
Describes the dominating soil type of the land fraction in the grid cell according to the following classes: 1: ice, 2: rock, 3: sand, 4:sandy loam, 5: loam, 6: loamy clay, 7: clay, 8: peat, 9: water.