From the last interglacial to the anthropocene - modeling a complete glacial cycle.
The PalMod project (https://www.palmod.de/) aims for a better understanding of how slow feedbacks in the Earth system
This data set is an ensemble reconstruction of volcanic stratospheric sulfur injection (VSSI) and stratospheric aerosol optical depth (SAOD) over the last 130,000 years that is based primarily on terrestrial
This simulation was performed to capture the global climate evolution of the last deglaciation. The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR). The model includes the spectral atmospheric model
This data collection offers one transient experiment and a set of future climate scenario experiments.
For the transient experiment the used model was integrated from a glacial state at 23 ka to the year
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
The transient simulation was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR) coupled to the ice-sheet model mPISM and the solid-earth
These set of future climate scenario experiments were performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR). The model includes the spectral