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
Other Authors: Villum Fonden
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2018
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683618788701
https://journals.sagepub.com/doi/pdf/10.1177/0959683618788701
https://journals.sagepub.com/doi/full-xml/10.1177/0959683618788701