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PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p3f1)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p1f2)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p7f2)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p6f2)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p5f2)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p2f1)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p4f2)
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... -
PalMod2 MPI-M MPI-ESM1-2-1-CR transient-deglaciation-interactive (r1i1p1f1)
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... -
PISM-VILMA glacial cycle simulations of the Antarctic Ice Sheet coupled to th...
The dynamics of the ice sheets on glacial time scales are highly controlled by interactions with the solid Earth, i.e., the glacial isostatic adjustment (GIA). Particularly at... -
Predicted relative sea-level and sea-level data for validation
We provide the model results of the manuscript "Glacial-isostatic adjustment models using geodynamically constrained 3D Earth structures" (Bagge et al. 2020, Paper) including...
