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...

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Bibliographic Details
Main Authors: E. Carnahan, G. Catania, T. C. Bartholomaus
Format: Article
Language:English
Published: Copernicus Publications 2022-10-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/16/4305/2022/tc-16-4305-2022.pdf