Responses of the Pine Island and Thwaites Glaciers to Melt and Sliding Parameterizations

The Pine Island and Thwaites glaciers are the two largest contributors to sea level rise from Antarctica. Here we examine the influence of basal friction and ice shelf basal melt in determining projected losses. We examine both Weertman and Coulomb friction laws with explicit weakening as the ice th...

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Bibliographic Details
Main Authors: Joughin, Ian, Shapero, Daniel, Dutrieux, Pierre
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2024
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/536632/
https://nora.nerc.ac.uk/id/eprint/536632/1/tc-18-2583-2024.pdf
https://tc.copernicus.org/articles/18/2583/2024/