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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- 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
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- 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: 04 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...
