The Existence of Multiple Steady States in the Flow of Large Ice Masses

Abstract We discuss the possibility of the occurrence of thermal instability in ice sheets and glaciers. This may arise from the non-linear viscous heating term, which could provide for the existence of multiple steady states in the flow and temperature fields: a word of warning is given about the a...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Fowler, A. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000010406
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010406
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Summary:Abstract We discuss the possibility of the occurrence of thermal instability in ice sheets and glaciers. This may arise from the non-linear viscous heating term, which could provide for the existence of multiple steady states in the flow and temperature fields: a word of warning is given about the applicability of these ideas.