A 2000-year record of ocean influence on Jakobshavn Isbræ calving activity, based on marine sediment cores
The Greenland Ice Sheet has experienced significant mass loss in recent years. A substantial component of this is attributable to the retreat of marine-terminating outlet glaciers, which lose mass through increases in calving, submarine melting and terrestrial meltwater discharge. In terms of iceber...
Published in: | The Holocene |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
SAGE Journals
2018
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/520710/ https://doi.org/10.1177/0959683618788701 |