Large and irreversible future decline of the Greenland ice sheet

<p>We have studied the evolution of the Greenland ice sheet under a range of constant climates typical of those projected for the end of the present century using a dynamical ice sheet model (Glimmer) coupled to an atmosphere general circulation model (FAMOUS–ice AGCM). The ice sheet surface m...

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Bibliographic Details
Main Authors: J. M. Gregory, S. E. George, R. S. Smith
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/14/4299/2020/tc-14-4299-2020.pdf