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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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation wi...
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... -
PalMod2 MPI-M MPI-ESM1-2-CR-CH4 future-methane
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).... -
PalMod2 MPI-M MPI-ESM1-2-CR-CH4 transient-deglaciation-prescribed-glac1d-methane
For transient-deglaciation-prescribed-glac1d-methane (r1i1p1f1): The transient experiment was performed with the Max Planck Institute for Meteorology Earth... -
Diatom percentage abundances for sediment core KH-10-7 COR1GC from the Conrad...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
Measured SC02 U/Th isotope activity ratios, calculated ages and monte-carlo d...
U-Th ages were calculated using the initial detrital 230Th/232Th value of 111 ± 41 ppm, which was previously calculated for SC02 based on two isochrons measured in separate... -
δ18O and δ13C at distance-from-top of stalagmite and Oxcal deposition model i...
Here are presented Mulu, Borneo (4°6'N, 114°53'E) Secret Cave stalagmite SC02 d18O and d13C values over Termination 1, published in Buckingham et al. (2022). This study reports... -
Clay mineralogical of sediment core HLY0501-01JPC from the Chukchi sea margin
This dataset has no description
