Glacier damage evolution over ice flow timescales

<p>The rate of mass loss from the Antarctic and Greenland ice sheets is controlled in large part by the processes of ice flow and ice fracture. Studies have shown these processes to be coupled: the development of fractured zones weakens the structural integrity of the ice, reducing ice viscosi...

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Bibliographic Details
Main Authors: M. Ranganathan, A. A. Robel, A. Huth, R. Duddu
Format: Article
Language:English
Published: Copernicus Publications 2025-04-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/19/1599/2025/tc-19-1599-2025.pdf
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