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)
The magnitude of the Antarctic ice sheet's contribution to global sea-level rise is dominated by the potential of its marine sectors to become unstable and collapse as a response to ocean (and atmospheric) forcing. This paper presents Antarctic sea-level response to sudden atmospheric and ocean...
Published in: | The Cryosphere |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Copernicus Publications
2017
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Online Access: | https://doi.org/10.5194/tc-11-1851-2017 https://www.the-cryosphere.net/11/1851/2017/tc-11-1851-2017.pdf https://doaj.org/article/71dabd4e60d8469884d065240702fdf3 |