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...

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Bibliographic Details
Main Authors: McCormack, F, Warner, R, Treverrow, A, Seroussi, H
Format: Conference Object
Language:English
Published: . 2019
Subjects:
Online Access:https://www.waisworkshop.org/workshop-2019#Agenda
http://ecite.utas.edu.au/135523