Interpreting englacial layer deformation in the presence of complex ice flow history with synthetic radargrams

Fast ice flow on the Antarctic continent constitutes much of the mass loss from the ice sheet. However, geophysical methods struggle to constrain ice flow history at depth, or separate the signatures of topography, ice dynamics and basal conditions on layer structure. We develop and demonstrate a me...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Cooper W. Elsworth, Dustin M. Schroeder, Matthew R. Siegfried
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2020
Subjects:
Online Access:https://doi.org/10.1017/aog.2019.41
https://doaj.org/article/8fff51a672d44bdf9e715bc7e320a178