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...

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Bibliographic Details
Main Authors: C. Schoof, A. D. Davis, T. V. Popa
Format: Article
Language:English
Published: Copernicus Publications 2017-10-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/11/2283/2017/tc-11-2283-2017.pdf