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: | 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 |
Similar Items
-
Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period
by: I. Tabone, et al.
Published: (2019-03-01) -
The Antarctic Ice Sheet response to glacial millennial-scale variability
by: J. Blasco, et al.
Published: (2019-01-01) -
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions
by: J. Blasco, et al.
Published: (2021-01-01) -
Simulating the Laurentide Ice Sheet of the Last Glacial Maximum
by: D. Moreno-Parada, et al.
Published: (2023-05-01) -
Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3
by: I. Tabone, et al.
Published: (2019-07-01)