Surface undulations of Antarctic ice streams tightly controlled by bedrock topography
Full Stokes flow-line models predict that fast-flowing ice streams transmit information about their bedrock topography most efficiently to the surface for basal undulations with length scales between 1 and 20 times the mean ice thickness. This typical behaviour is independent of the precise values o...
Published in: | The Cryosphere |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-7-407-2013 https://tc.copernicus.org/articles/7/407/2013/ |