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...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: McCormack, FS, Warner, RC, Seroussi, H, Dow, CF, Roberts, JL, Treverrow, A
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell Publishing Inc. 2022
Subjects:
Online Access:https://doi.org/10.1029/2021JF006332
http://ecite.utas.edu.au/154118