Observed mechanism for sustained glacier retreat and acceleration in response to ocean warming around Greenland
<p>The dynamic loss of ice via outlet glaciers around the Greenland Ice Sheet is a major contributor to sea level rise. However, the retreat history and ensuing dynamic mass loss of neighboring glaciers are disparate, complicating projections of sea level rise. Here, we examine the stress bala...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2022-10-01
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Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/16/4305/2022/tc-16-4305-2022.pdf |