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 marineterminating outlet glaciers, which lose mass through increases in calving, submarine melting and terrestrial meltwater discharge. In terms of iceberg...

Full description

Bibliographic Details
Published in:The Holocene
Main Authors: WANGNER, David, JENNINGS, Anne, VERMASSEN, Flor, DYKE, Laurence, HOGAN, Kelly, SCHMIDT, Sabine, KJÆR, Kurt, KNUDSEN, Mads, ANDRESEN, Camilla
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Disko Bugt
foraminifera
Greenland
Holocene
ice-rafted debris
Jakobshavn Isbræ
palaeoclimatology
West Greenland Current
Planète et Univers [physics]/Océan
Atmosphère
Isfjord
Jakobshavn Isfjord
Disko bugt
glacier
Ice Sheet
Jakobshavn
Jakobshavn isbræ
Sea ice
Online Access:https://oskar-bordeaux.fr/handle/20.500.12278/199955
https://hdl.handle.net/20.500.12278/199955
https://doi.org/10.1177/0959683618788701

Similar Items