Articles | Volume 20, issue 4
https://doi.org/10.5194/cp-20-865-2024
https://doi.org/10.5194/cp-20-865-2024
Research article
 | 
08 Apr 2024
Research article |  | 08 Apr 2024

Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation

Nils Weitzel, Heather Andres, Jean-Philippe Baudouin, Marie-Luise Kapsch, Uwe Mikolajewicz, Lukas Jonkers, Oliver Bothe, Elisa Ziegler, Thomas Kleinen, André Paul, and Kira Rehfeld

Data sets

PalMod 130k marine palaeoclimate data synthesis version 1.1.1 L. Jonkers et al. https://doi.org/10.5281/zenodo.7785766

PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation with prescribed ice sheets from GLAC-1D reconstructions (r1i1p3f2) U. Mikolajewicz et al. https://doi.org/10.26050/WDCC/PMMXMCRTDGP132

PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation with prescribed ice sheets from ICE-6G reconstructions (r1i1p3f2) U. Mikolajewicz et al. https://doi.org/10.26050/WDCC/PMMXMCRTDIP132

PalMod2 MPI-M MPI-ESM1-2-CR Transient Simulations of the Last Deglaciation with prescribed ice sheets from ICE-6G reconstructions (r1i1p2f2) U. Mikolajewicz et al. https://doi.org/10.26050/WDCC/PMMXMCRTDIP122

PalMod2 MPI-M MPI-ESM1-2-CR-CH4 transient-deglaciation-prescribed-glac1d-methane T. Kleinen et al. https://doi.org/10.26050/WDCC/PMMXMCHTD

QUEST Quaternary: FAMOUS glacial cycle model data T. Lenton https://catalogue.ceda.ac.uk/uuid/a43dcfaccfae4824ab9ab2b572703e72

Model code and software

Code in support of "Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation" N. Weitzel et al. https://doi.org/10.5281/zenodo.10497834

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Short summary
The ability of climate models to faithfully reproduce past warming episodes is a valuable test considering potentially large future warming. We develop a new method to compare simulations of the last deglaciation with temperature reconstructions. We find that reconstructions differ more between regions than simulations, potentially due to deficiencies in the simulation design, models, or reconstructions. Our work is a promising step towards benchmarking simulations of past climate transitions.