Force balance along Isunnguata Sermia, west Greenland

Ice flows when gravity acts on gradients in surface elevation, producing driving stresses. In the Isunnguata Sermia and Russel Glacier catchments of western Greenland, a 50% decline in driving stress along a flow line is juxtaposed with increasing surface flow speed. Here, these circumstances are in...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Toby Meierbachtol, Joel Harper, Jesse Johnson
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2016
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2016.00087
https://doaj.org/article/aa8c515ecae848bc934c3b963bd83916