Ice stream or not? Radio-echo sounding of Carlson Inlet, West Antarctica

The Antarctic Ice Sheet loses mass to the surrounding ocean mainly by drainage through a network of ice streams: fast-flowing glaciers bounded on either side by ice flowing one or two orders of magnitude more slowly. Ice streams flow despite low driving stress because of low basal resistance but are...

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Bibliographic Details
Published in:The Cryosphere
Main Author: E. C. King
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/tc-5-907-2011
https://doaj.org/article/33428e6dffc842d8993a3a1656be2a7e