The Dynamics of Marine Ice Sheets

Abstract Marine ice sheets rest on land that, for the most part, is below sea-level. Ice that flows across the grounding line, where the ice sheet becomes afloat, either calves into icebergs or forms a floating ice shelf joined to the ice sheet. At the grounding line there is a transition from ice-s...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Thomas, Robert H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014726
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014726