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...
Published in: | Annals of Glaciology |
---|---|
Main Authors: | , , |
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 |