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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65 citations as recorded by crossref.
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65 citations as recorded by crossref.
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- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. https://doi.org/10.1029/2020JF005827
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- Investigating the internal structure of the Antarctic ice sheet: the utility of isochrones for spatiotemporal ice-sheet model calibration J. Sutter et al. https://doi.org/10.5194/tc-15-3839-2021
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- Modeling the climate sensitivity of Patagonian glaciers and their responses to climatic change during the global last glacial maximum Q. Yan et al. https://doi.org/10.1016/j.quascirev.2022.107582
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- A seismic proxy identifying the transition to an ice sheet polar regime from the sedimentary sequence on the George V Land continental margin (Antarctica) B. Giuliano et al. https://doi.org/10.1016/j.palaeo.2025.113393
- Response of the East Antarctic Ice Sheet to past and future climate change C. Stokes et al. https://doi.org/10.1038/s41586-022-04946-0
- Radar isochrones as constraints on paleo–ice-sheet model simulations in two off-divide regions of East Antarctica J. Bodart et al. https://doi.org/10.5194/tc-20-1379-2026
- Petrographic signature of the gravel fraction from late Quaternary glacigenic sediments in the Ross Sea (Antarctica): Implications for source terranes and Neogene glacial reconstructions M. Perotti et al. https://doi.org/10.1016/j.sedgeo.2024.106742
- Bathymetry-constrained impact of relative sea-level change on basal melting in Antarctica M. Kreuzer et al. https://doi.org/10.5194/tc-19-1181-2025
- Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 1: Boundary conditions and climatic forcing T. Albrecht et al. https://doi.org/10.5194/tc-14-599-2020
- Investigating the impact of sub-ice shelf melt on Antarctic ice sheet spin-up and projections F. Gao et al. https://doi.org/10.5194/tc-20-1947-2026
- A thinner-than-present West Antarctic Ice Sheet in the southern Weddell Sea Embayment during the Holocene D. Small et al. https://doi.org/10.5194/tc-20-2035-2026
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. https://doi.org/10.1038/s43017-022-00309-5
Saved (final revised paper)
Latest update: 21 Sep 2026
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...
