Simulating the Holocene deglaciation across a marine-terminating portion of southwestern Greenland in response to marine and atmospheric forcings

<p>Numerical simulations of the Greenland Ice Sheet (GrIS) over geologic timescales can greatly improve our knowledge of the critical factors driving GrIS demise during climatically warm periods, which has clear relevance for better predicting GrIS behavior over the upcoming centuries. To ass...

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Bibliographic Details
Main Authors: J. K. Cuzzone, N. E. Young, M. Morlighem, J. P. Briner, N.-J. Schlegel
Format: Article
Language:English
Published: Copernicus Publications 2022-06-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/16/2355/2022/tc-16-2355-2022.pdf