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We develop a self-consistent, large ensemble, high-resolution, bias-corrected global dataset of future climates for a set of four possible 21st century scenarios, which is suitable for assessing local-scale
The experiment includes the source code, compile and run scripts for ICON-ESM-V1.0 in the configuration “Ruby-0”, the initialization data for ICON-ESM-V1 in the configuration “Ruby-0”, and scripts, libraries, and input data used to produce figures.
Source code of the Max Planck Institute Earth System Model (MPI-ESM1.2) adopted to the project PRIMAVERA for the comparison of four different ocean vertical mixing schemes.
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. Long-term stabilization of the atmospheric pCO2 simulations. The atmospheric pCO2 is prescribed to rise exponentially