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 oc...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2017-08-01
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| Series: | The Cryosphere |
| Online Access: | https://www.the-cryosphere.net/11/1851/2017/tc-11-1851-2017.pdf |