Tidally induced velocity variations of the Beardmore Glacier, Antarctica, and their representation in satellite measurements of ice velocity
Ocean tides close to the grounding line of outlet glaciers around Antarctica have been shown to directly influence ice velocity, both linearly and non-linearly. These fluctuations can be significant and have the potential to affect satellite measurements of ice discharge, which assume displacement b...
Main Authors: | O. J. Marsh, W. Rack, D. Floricioiu, N. R. Golledge, W. Lawson |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2013-09-01
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Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/7/1375/2013/tc-7-1375-2013.pdf |
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