Articles | Volume 11, issue 4
https://doi.org/10.5194/tc-11-1851-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-1851-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
08 Aug 2017
Research article |
| 08 Aug 2017
Sea-level response to melting of Antarctic ice shelves on multi-centennial timescales with the fast Elementary Thermomechanical Ice Sheet model (f.ETISh v1.0)
Laboratoire de Glaciologie, Department of Geosciences, Environment and
Society, Université libre de Bruxelles, Av. F.D. Roosevelt
50, 1050 Brussels, Belgium
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66 citations as recorded by crossref.
- Basal melting of Ross Ice Shelf from solar heat absorption in an ice-front polynya C. Stewart et al. 10.1038/s41561-019-0356-0
- Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2) A. Levermann et al. 10.5194/esd-11-35-2020
- Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing E. Kazmierczak et al. 10.5194/tc-16-4537-2022
- Compensating errors in inversions for subglacial bed roughness: same steady state, different dynamic response C. Berends et al. 10.5194/tc-17-1585-2023
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- PARASO, a circum-Antarctic fully coupled ice-sheet–ocean–sea-ice–atmosphere–land model involving f.ETISh1.7, NEMO3.6, LIM3.6, COSMO5.0 and CLM4.5 C. Pelletier et al. 10.5194/gmd-15-553-2022
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- Variations of the Antarctic Ice Sheet in a Coupled Ice Sheet‐Earth‐Sea Level Model: Sensitivity to Viscoelastic Earth Properties D. Pollard et al. 10.1002/2017JF004371
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- ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century H. Seroussi et al. 10.5194/tc-14-3033-2020
- Mapping geodetically inferred Antarctic ice surface height changes into thickness changes: a sensitivity study N. Valencic et al. 10.5194/tc-18-2969-2024
- Grounding-line flux formula applied as a flux condition in numerical simulations fails for buttressed Antarctic ice streams R. Reese et al. 10.5194/tc-12-3229-2018
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- Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP) S. Sun et al. 10.1017/jog.2020.67
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- A rapidly converging initialisation method to simulate the present-day Greenland ice sheet using the GRISLI ice sheet model (version 1.3) S. Le clec'h et al. 10.5194/gmd-12-2481-2019
- Quantifying the potential future contribution to global mean sea level from the Filchner–Ronne basin, Antarctica E. Hill et al. 10.5194/tc-15-4675-2021
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- 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
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- Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling B. Van Liefferinge et al. 10.5194/tc-12-2773-2018
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- The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
- Large Earthquakes in Subduction Zones around the Polar Regions as a Possible Reason for Rapid Climate Warming in the Arctic and Glacier Collapse in West Antarctica L. Lobkovsky et al. 10.3390/geosciences13060171
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- The Utrecht Finite Volume Ice-Sheet Model: UFEMISM (version 1.0) C. Berends et al. 10.5194/gmd-14-2443-2021
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- A comparison of the stability and performance of depth-integrated ice-dynamics solvers A. Robinson et al. 10.5194/tc-16-689-2022
- Statistical emulation of a perturbed basal melt ensemble of an ice sheet model to better quantify Antarctic sea level rise uncertainties M. Berdahl et al. 10.5194/tc-15-2683-2021
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- The Large Earthquakes and Deformation Waves as Possible Triggers of Climate Warming in the Arctic and Glacier Destruction in the Antarctic L. Lobkovskii et al. 10.31857/S0869587323060117
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- Acceleration of Antarctica glaciers at high subglacial heat flow L. Lobkovsky et al. 10.31857/S2686739724030203
- ATAT 1.1, the Automated Timing Accordance Tool for comparing ice-sheet model output with geochronological data J. Ely et al. 10.5194/gmd-12-933-2019
- Brief communication: On calculating the sea-level contribution in marine ice-sheet models H. Goelzer et al. 10.5194/tc-14-833-2020
- Antarctic ice dynamics amplified by Northern Hemisphere sea-level forcing N. Gomez et al. 10.1038/s41586-020-2916-2
- FastIsostasy v1.0 – a regional, accelerated 2D glacial isostatic adjustment (GIA) model accounting for the lateral variability of the solid Earth J. Swierczek-Jereczek et al. 10.5194/gmd-17-5263-2024
- The Paris Climate Agreement and future sea-level rise from Antarctica R. DeConto et al. 10.1038/s41586-021-03427-0
- The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing I. Tabone et al. 10.5194/cp-14-455-2018
- A kinematic formalism for tracking ice–ocean mass exchange on the Earth's surface and estimating sea-level change S. Adhikari et al. 10.5194/tc-14-2819-2020
- Contrasting Response of West and East Antarctic Ice Sheets to Glacial Isostatic Adjustment V. Coulon et al. 10.1029/2020JF006003
- The circum-Antarctic ice-shelves respond to a more positive Southern Annular Mode with regionally varied melting D. Verfaillie et al. 10.1038/s43247-022-00458-x
- Bed topography and marine ice-sheet stability O. Sergienko & D. Wingham 10.1017/jog.2021.79
- Understanding of Contemporary Regional Sea‐Level Change and the Implications for the Future B. Hamlington et al. 10.1029/2019RG000672
2 citations as recorded by crossref.
Discussed (final revised paper)
Discussed (final revised paper)
Discussed (preprint)
Latest update: 24 Apr 2025
Short summary
Marine Ice Sheet Instability is a mechanism that can potentially lead to collapse of marine sectors of the Antarctic ice sheet and floating ice shelves play a crucial role herein. Improved grounding line physics (interaction with subglacial sediment) are implemented in a new ice-sheet model and compared to traditional sliding laws. Ice shelf collapse leads to a significant higher sea-level contribution (up to 15 m in 500 years) compared to traditional grounding-line approaches.
Marine Ice Sheet Instability is a mechanism that can potentially lead to collapse of marine...
