Boundary layer models for calving marine outlet glaciers
We consider the flow of marine-terminating outlet glaciers that are laterally confined in a channel of prescribed width. In that case, the drag exerted by the channel side walls on a floating ice shelf can reduce extensional stress at the grounding line. If ice flux through the grounding line inc...
Main Authors: | C. Schoof, A. D. Davis, T. V. Popa |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-10-01
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Series: | The Cryosphere |
Online Access: | https://www.the-cryosphere.net/11/2283/2017/tc-11-2283-2017.pdf |
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