Articles | Volume 14, issue 2
https://doi.org/10.5194/tc-14-633-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-633-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Feb 2020
Research article |
| 14 Feb 2020
| 14 Feb 2020
Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 601203, 14412 Potsdam, Germany
Ricarda Winkelmann
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 601203, 14412 Potsdam, Germany
University of Potsdam, Institute of Physics and Astronomy,
Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany
Anders Levermann
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 601203, 14412 Potsdam, Germany
University of Potsdam, Institute of Physics and Astronomy,
Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany
Lamont-Doherty Earth Observatory, Columbia University, New York, USA
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- GEORGIA: A Graph Neural Network Based EmulatOR for Glacial Isostatic Adjustment Y. Lin et al. 10.1029/2023GL103672
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- RETRACTED: Sea-level fingerprinting technique: A window into meltwater pulse 1 A and constraints from Antarctica W. Baba & J. Pattanaik 10.1016/j.gloplacha.2025.104793
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Latest update: 03 Nov 2025
Short summary
A large ensemble of glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) was analyzed in which four relevant model parameters were systematically varied. These parameters were selected in a companion study and are associated with uncertainties in ice dynamics, climatic forcing, basal sliding and solid Earth deformation. For each ensemble member a statistical score is computed, which enables calibrating the model against both modern and geologic data.
A large ensemble of glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice...
