Articles | Volume 14, issue 2
https://doi.org/10.5194/tc-14-599-2020
© 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-14-599-2020
© 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 1: Boundary conditions and climatic forcing
Torsten Albrecht
CORRESPONDING AUTHOR
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
Institute of Physics and Astronomy, University of Potsdam,
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
Institute of Physics and Astronomy, University of Potsdam,
Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany
Lamont-Doherty Earth Observatory, Columbia University, New York, USA
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Cited
30 citations as recorded by crossref.
- PISM-LakeCC: Implementing an adaptive proglacial lake boundary in an ice sheet model S. Hinck et al. 10.5194/tc-16-941-2022
- 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
- Glacial isostatic adjustment and post-seismic deformation in Antarctica W. van der Wal et al. 10.1144/M56-2022-13
- 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 evolution of future Antarctic surface melt using PISM-dEBM-simple J. Garbe et al. 10.5194/tc-17-4571-2023
- Sensitivity of the Antarctic ice sheets to the warming of marine isotope substage 11c M. Mas e Braga et al. 10.5194/tc-15-459-2021
- Southern Ocean sea surface temperature synthesis: Part 2. Penultimate glacial and last interglacial D. Chandler & P. Langebroek 10.1016/j.quascirev.2021.107190
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
- Hysteretic evolution of ice rises and ice rumples in response to variations in sea level A. Henry et al. 10.5194/tc-16-3889-2022
- Range of 21st century ice mass changes in the Filchner-Ronne region of Antarctica A. Johnson et al. 10.1017/jog.2023.10
- Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis T. Albrecht et al. 10.5194/tc-14-633-2020
- Diversity of pollen grains transported from South America to the Antarctic Peninsula through atmospheric dispersal L. Rodrigues et al. 10.1007/s00300-023-03165-1
- The hysteresis of the Antarctic Ice Sheet J. Garbe et al. 10.1038/s41586-020-2727-5
- 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
- Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP) S. Sun et al. 10.1017/jog.2020.67
- Brief communication: On calculating the sea-level contribution in marine ice-sheet models H. Goelzer et al. 10.5194/tc-14-833-2020
- 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
- Coupling framework (1.0) for the PISM (1.1.4) ice sheet model and the MOM5 (5.1.0) ocean model via the PICO ice shelf cavity model in an Antarctic domain M. Kreuzer et al. 10.5194/gmd-14-3697-2021
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning Maud Land, East Antarctica Y. Suganuma et al. 10.1038/s43247-022-00599-z
- 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 inter-annual temperature variability on the Greenland Ice Sheet volume M. Lauritzen et al. 10.1017/aog.2023.53
- Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks M. Zeitz et al. 10.5194/esd-13-1077-2022
- 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
- Antarctic Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions J. Blasco et al. 10.5194/tc-15-215-2021
- Compensating errors in inversions for subglacial bed roughness: same steady state, different dynamic response C. Berends et al. 10.5194/tc-17-1585-2023
- Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks M. Willeit et al. 10.5194/cp-20-597-2024
30 citations as recorded by crossref.
- PISM-LakeCC: Implementing an adaptive proglacial lake boundary in an ice sheet model S. Hinck et al. 10.5194/tc-16-941-2022
- 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
- Glacial isostatic adjustment and post-seismic deformation in Antarctica W. van der Wal et al. 10.1144/M56-2022-13
- 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 evolution of future Antarctic surface melt using PISM-dEBM-simple J. Garbe et al. 10.5194/tc-17-4571-2023
- Sensitivity of the Antarctic ice sheets to the warming of marine isotope substage 11c M. Mas e Braga et al. 10.5194/tc-15-459-2021
- Southern Ocean sea surface temperature synthesis: Part 2. Penultimate glacial and last interglacial D. Chandler & P. Langebroek 10.1016/j.quascirev.2021.107190
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
- Hysteretic evolution of ice rises and ice rumples in response to variations in sea level A. Henry et al. 10.5194/tc-16-3889-2022
- Range of 21st century ice mass changes in the Filchner-Ronne region of Antarctica A. Johnson et al. 10.1017/jog.2023.10
- Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis T. Albrecht et al. 10.5194/tc-14-633-2020
- Diversity of pollen grains transported from South America to the Antarctic Peninsula through atmospheric dispersal L. Rodrigues et al. 10.1007/s00300-023-03165-1
- The hysteresis of the Antarctic Ice Sheet J. Garbe et al. 10.1038/s41586-020-2727-5
- 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
- Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP) S. Sun et al. 10.1017/jog.2020.67
- Brief communication: On calculating the sea-level contribution in marine ice-sheet models H. Goelzer et al. 10.5194/tc-14-833-2020
- 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
- Coupling framework (1.0) for the PISM (1.1.4) ice sheet model and the MOM5 (5.1.0) ocean model via the PICO ice shelf cavity model in an Antarctic domain M. Kreuzer et al. 10.5194/gmd-14-3697-2021
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning Maud Land, East Antarctica Y. Suganuma et al. 10.1038/s43247-022-00599-z
- 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 inter-annual temperature variability on the Greenland Ice Sheet volume M. Lauritzen et al. 10.1017/aog.2023.53
- Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks M. Zeitz et al. 10.5194/esd-13-1077-2022
- 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
- Antarctic Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions J. Blasco et al. 10.5194/tc-15-215-2021
- Compensating errors in inversions for subglacial bed roughness: same steady state, different dynamic response C. Berends et al. 10.5194/tc-17-1585-2023
- Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks M. Willeit et al. 10.5194/cp-20-597-2024
Discussed (final revised paper)
Latest update: 24 Apr 2024
Short summary
During the last glacial cycles the Antarctic Ice Sheet experienced alternating climatic conditions and varying sea-level history. In response, changes in ice sheet volume and ice-covered area occurred, implying feedbacks on the global sea level. We ran model simulations of the ice sheet with the Parallel Ice Sheet Model (PISM) over the last two glacial cycles to evaluate the model's sensitivity to different choices of boundary conditions and parameters to gain confidence for future projections.
During the last glacial cycles the Antarctic Ice Sheet experienced alternating climatic...
