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...
Published in: | The Cryosphere |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-13-723-2019 https://doaj.org/article/9b66c0fc80d54fa791bcda2c3b459090 |