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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Bibliographic Details
Main Author: F. Pattyn
Format: Article
Language:English
Published: Copernicus Publications 2017-08-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/11/1851/2017/tc-11-1851-2017.pdf

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