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...
Published in: | The Cryosphere |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Coperincus
2018
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Subjects: | |
Online Access: | https://nrl.northumbria.ac.uk/id/eprint/37704/ https://doi.org/10.5194/tc-12-3907-2018 https://nrl.northumbria.ac.uk/id/eprint/37704/1/tc-12-3907-2018.pdf |