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...

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Bibliographic Details
Published in:The Holocene
Main Authors: Wangner, David J., Jennings, Anne E., Vermassen, Flor, Dyke, Laurence M., Hogan, Kelly A., Schmidt, Sabine, Kjær, Kurt H., Knudsen, Mads F., Andresen, Camilla S.
Format: Article in Journal/Newspaper
Language:unknown
Published: SAGE Journals 2018
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/520710/
https://doi.org/10.1177/0959683618788701