Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events.

Dynamic ice discharge from outlet glaciers across the Greenland ice sheet has increased since the beginning of the 21st century. Calving from floating ice tongues that buttress these outlets can accelerate ice flow and discharge of grounded ice. However, little is known about the dynamic impact of i...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Hill, E.A., Hilmar Gudmundsson, G., Carr, R.J., Stokes, C.R.
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus Publications 2018
Subjects:
Online Access:http://dro.dur.ac.uk/26945/
http://dro.dur.ac.uk/26945/1/26945.pdf
http://dro.dur.ac.uk/26945/2/26945.pdf
https://doi.org/10.5194/tc-12-3907-2018