Physical Conditions of Fast Glacier Flow:2. Variable Extent of Anisotropic Ice and Soft Basal Sediment From Seismic Reflection Data Acquired on Store Glacier, West Greenland

Outlet glaciers of the Greenland Ice Sheet transport ice from the interior to the ocean and contribute directly to sea level rise because discharge and ablation often exceed the accumulation. To develop a better understanding of these fast-flowing glaciers, we investigate the basal conditions of Sto...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Hofstede, C., Christoffersen, P., Hubbard, B., Doyle, S. H., Young, T. J., Diez, A., Eisen, O., Hubbard, A.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
anisotropy
deformation
patches
seismic
sliding
subglacial
Greenland
Uummannaq Fjord
glacier
Ice Sheet
Uummannaq
Online Access:https://research-portal.st-andrews.ac.uk/en/researchoutput/physical-conditions-of-fast-glacier-flow(d8aa1282-4744-4bfb-9dd3-07d665981547).html
https://doi.org/10.1002/2017JF004297
http://www.scopus.com/inward/record.url?scp=85042441998&partnerID=8YFLogxK

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