This is a hydrodynamic hindcast for the North Sea and the Northeast Atlantic over the period 1948-2022 and ongoing. Atmospheric forcing is the regional COSMO-CLM NCEP1 data. The simulation has been performed
This is a hydrodynamic hindcast for the North Sea and the Northeast Atlantic over the period 1995-2019. Atmospheric forcing is COSMO-REA6 high-resolution reconstruction (https://reanalysis.meteo.uni-bonn.de/?COSMO-REA6).
These are the hydrodynamic transient scenarios for the North Sea and the Northeast Atlantic for the period 1950-2006 (historical) and 2006-2100 (future). Atmospheric forcing originates from CMIP5 CORDEX
The hydrodynamic model TRIM-NP in a barotropic mode is used to simulate the strong storm tide in March 1906 forced by NOAA-CIRES-DOE Twentieth Century Reanalysis (20CR) version 2c and 3. datasets (https://portal.nersc.gov/project/20C_Reanalysis/).
The hydrodynamic model TRIM-NP in a barotropic mode is used to simulate the strong storm tide in March 1906 forced by reconstructed weather data by the Deutsche Wetterdienst (DWD) and Helmholtz-Zentrum
The hydrodynamic model TRIM-NP in a barotropic mode is used to simulate the strong storm tide in March 1906 forced by ECMWF ERA-20C and CERA-20C ensemble of coupled climate reanalyses (https://www.ecmwf.int).
These are the hydrodynamic transient scenarios for the North Sea and the Northeast Atlantic for the period 1950-2006 (historical) and 2006-2100 (RCP2.6 and RCP8.5). Atmospheric forcing is CMIP5 MOHC-HadGEM2-ES
These are the hydrodynamic transient scenarios for the North Sea and the Northeast Atlantic for the period 1950-2006 (historical) and 2006-2100 (RCP2.6 and RCP8.5). Atmospheric forcing is CMIP5 MPI-M-MPI-ESM-LR
This group contains hourly model results of all members of this regional climate ensemble for the RCP8.5 period 2006-2099. Simulations are continuations of each ensemble member, which differ only due to
This group contains hourly model results of all members of this regional climate ensemble for the historical period 1950-2005. Members of the ensemble differ only due to different initial conditions.
This group contains hourly model results of this regional climate simulation with pre-industrial atmospheric pCO2 of year 1850 for the period 1950-2099. Available data: (a) ocean model results of sea