Historical simulation with REMO2020-2-iMOVE performed on the EURO-CORDEX domain at 0.11 degree resolution, using MPI-ESM1-2-HR data as lateral boundary conditions for the years 1950-2014, using static
Scenario simulation with REMO2020-2-iMOVE performed on the EURO-CORDEX domain at 0.11 degree resolution, using MPI-ESM1-2-HR SSP 126 data as lateral boundary conditions for the years 2014-2100, using static
Historical simulation with REMO2020-2-iMOVE-LUC performed on the EURO-CORDEX domain at 0.11 degree resolution, using MPI-ESM1-2-HR data as lateral boundary conditions for the years 1950-2014, with annual
SSP126 simulation with REMO2020-2-iMOVE-LUC performed on the EURO-CORDEX domain at 0.11 degree resolution, using MPI-ESM1-2-HR SSP126 data as lateral boundary conditions for the years 2015-2100, with annual
Evaluation simulation with REMO2020-2-iMOVE performed on the EURO-CORDEX domain at 0.11 degree resolution, using ERA5.1 reanalysis data as lateral boundary conditions for the years 1981-2020, using static
Evaluation simulation with REMO2020-2-iMOVE-LUC performed on the EURO-CORDEX domain at 0.11 degree resolution, using ERA5.1 reanalysis data as lateral boundary conditions for the years 1981-2020, with
Building upon on-going large, integrated projects (THRESHOLDS and DAMOCLES FP6 IPs, and the ARCTOS network) the project Arctic Tipping Points (ATP) aimed at identifying the elements of the Arctic marine
The regional climate model REMO has been used to simulate future climate of Germany for different climate scenarios (IPCC). The simulations have been initiated by Umweltbundesamt (P. Mahrenholz) and performed