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: | , , , , , , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
SAGE Publications
2018
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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 |