The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing
Observations suggest that during the last decades the Greenland Ice Sheet (GrIS) has experienced a gradually accelerating mass loss, in part due to the observed speed-up of several of Greenland's marine-terminating glaciers. Recent studies directly attribute this to warming North Atlantic t...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-04-01
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Series: | Climate of the Past |
Online Access: | https://www.clim-past.net/14/455/2018/cp-14-455-2018.pdf |