Changing basal conditions during the speed-up of Jakobshavn Isbræ, Greenland

Ice-sheet outlet glaciers can undergo dynamic changes such as the rapid speed-up of Jakobshavn Isbræ following the disintegration of its floating ice tongue. These changes are associated with stress changes on the boundary of the ice mass. We invert for basal conditions from surface velocity data th...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Habermann, M., Truffer, M., Maxwell, D.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/tc-7-1679-2013
https://noa.gwlb.de/receive/cop_mods_00021152
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00021107/tc-7-1679-2013.pdf
https://tc.copernicus.org/articles/7/1679/2013/tc-7-1679-2013.pdf