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...
Published in: | The Cryosphere |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2024
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-18-2583-2024 https://noa.gwlb.de/receive/cop_mods_00073880 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072020/tc-18-2583-2024.pdf https://tc.copernicus.org/articles/18/2583/2024/tc-18-2583-2024.pdf |