The internal deformation regime of Thwaites Glacier
Internal deformation is the main process controlling ice flow in ice shelves and inslow-moving regions of polar ice sheets where the ice is frozen to the bed. However, thecontribution of internal deformation to flow in ice streams and fast-flowing regions is typicallypoorly constrained in ice sheet...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | English |
Published: |
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2019
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Subjects: | |
Online Access: | https://www.waisworkshop.org/workshop-2019#Agenda http://ecite.utas.edu.au/135523 |