Modeling the response of northwest Greenland to enhanced ocean thermal forcing and subglacial discharge

Calving-front dynamics is an important control on Greenland's ice mass balance. Ice front retreat of marine-terminating glaciers may, for example, lead to a loss in resistive stress, which ultimately results in glacier acceleration and thinning. Over the past decade, it has been suggested that...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: M. Morlighem, M. Wood, H. Seroussi, Y. Choi, E. Rignot
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-13-723-2019
https://doaj.org/article/9b66c0fc80d54fa791bcda2c3b459090