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...

Full description

Bibliographic Details
Main Authors: I. Tabone, J. Blasco, A. Robinson, J. Alvarez-Solas, M. Montoya
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:Climate of the Past
Online Access:https://www.clim-past.net/14/455/2018/cp-14-455-2018.pdf