Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams

Flow of glacial ice in the West Antarctic Ice Sheet localizes in narrow bands of fast-flowing ice streams bordered by ridges of nearly stagnant ice, but our understanding of the physical processes that generate this morphology is incomplete. Here we study the thermal and mechanical properties of ice...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Suckale, Jenny, Platt, John Daniel, Perol, Thibaut, Rice, James Robert
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2014
Subjects:
Online Access:http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315
https://doi.org/10.1002/2013jf003008