Dynamical processes involved in the retreat of marine ice sheets

Marine ice sheets with mechanics described by the shallow-ice approximation by definition do not couple mechanically with the shelf. Such ice sheets are known to have neutral equilibria. We consider the implications of this for their dynamics and in particular for mechanisms which promote marine ice...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Hindmarsh, Richard C.A., Le Meur, E.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2001
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/19614/