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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32 citations as recorded by crossref.
- Overshooting the critical threshold for the Greenland ice sheet N. Bochow et al. 10.1038/s41586-023-06503-9
- Modeling the climate sensitivity of Patagonian glaciers and their responses to climatic change during the global last glacial maximum Q. Yan et al. 10.1016/j.quascirev.2022.107582
- Simulating the Laurentide Ice Sheet of the Last Glacial Maximum D. Moreno-Parada et al. 10.5194/tc-17-2139-2023
- Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica J. Johnson et al. 10.5194/tc-16-1543-2022
- New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica J. Adams et al. 10.5194/tc-16-4887-2022
- Polarfuchs (Kolumne): Die Antarktis im Computer – wie funktionieren Computermodelle? L. Nicola 10.5194/polf-91-105-2023
- 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. 10.1029/2020JF005827
- The influence of emissions scenarios on future Antarctic ice loss is unlikely to emerge this century D. Lowry et al. 10.1038/s43247-021-00289-2
- Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream T. Gerber et al. 10.1038/s41467-023-38139-8
- Description and validation of the ice-sheet model Yelmo (version 1.0) A. Robinson et al. 10.5194/gmd-13-2805-2020
- Modelling Last Glacial Maximum ice cap with the Parallel Ice Sheet Model to infer palaeoclimate in south‐west Turkey A. Candaş et al. 10.1002/jqs.3239
- Abrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment M. Grieman et al. 10.1038/s41561-024-01375-8
- Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea T. Hillebrand et al. 10.5194/tc-15-3329-2021
- Geothermal heat flux is the dominant source of uncertainty in englacial-temperature-based dating of ice rise formation A. Montelli & J. Kingslake 10.5194/tc-17-195-2023
- Strategies for regional modeling of surface mass balance at the Monte Sarmiento Massif, Tierra del Fuego F. Temme et al. 10.5194/tc-17-2343-2023
- Glacial isostatic adjustment and post-seismic deformation in Antarctica W. van der Wal et al. 10.1144/M56-2022-13
- A Greenland-wide empirical reconstruction of paleo ice sheet retreat informed by ice extent markers: PaleoGrIS version 1.0 T. Leger et al. 10.5194/cp-20-701-2024
- The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded R. Reese et al. 10.5194/tc-17-3761-2023
- Last-glacial-cycle glacier erosion potential in the Alps J. Seguinot & I. Delaney 10.5194/esurf-9-923-2021
- An ensemble of Antarctic deglacial simulations constrained by geological observations M. Pittard et al. 10.1016/j.quascirev.2022.107800
- The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model R. Reese et al. 10.5194/tc-14-3097-2020
- Range of 21st century ice mass changes in the Filchner-Ronne region of Antarctica A. Johnson et al. 10.1017/jog.2023.10
- A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting Y. Lin et al. 10.1038/s41467-021-21990-y
- Quantifying the effect of ocean bed properties on ice sheet geometry over 40 000 years with a full-Stokes model C. Schannwell et al. 10.5194/tc-14-3917-2020
- Revisiting temperature sensitivity: how does Antarctic precipitation change with temperature? L. Nicola et al. 10.5194/tc-17-2563-2023
- Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. 10.5194/tc-15-4929-2021
- GEORGIA: A Graph Neural Network Based EmulatOR for Glacial Isostatic Adjustment Y. Lin et al. 10.1029/2023GL103672
- Response of the East Antarctic Ice Sheet to past and future climate change C. Stokes et al. 10.1038/s41586-022-04946-0
- A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
- 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. 10.5194/tc-14-599-2020
- Investigating the internal structure of the Antarctic ice sheet: the utility of isochrones for spatiotemporal ice-sheet model calibration J. Sutter et al. 10.5194/tc-15-3839-2021
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
Latest update: 25 Apr 2024
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...
