Modeling the deformation regime of Thwaites Glacier, West Antarctica, using a simple flow relation for ice anisotropy (ESTAR)
Ice deformation dominates the evolution of ice shelf flow and the slow-moving regions in theinterior of ice sheets. However, deformation may be poorly represented in large-scale ice sheet models thatuse the Glen flow relation, due to its questionable applicability to the steady-state flow of anisotr...
Published in: | Journal of Geophysical Research: Earth Surface |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley-Blackwell Publishing Inc.
2022
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Subjects: | |
Online Access: | https://doi.org/10.1029/2021JF006332 http://ecite.utas.edu.au/154118 |