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...
Published in: | Frontiers in Earth Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media S.A.
2016
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Subjects: | |
Online Access: | https://doi.org/10.3389/feart.2016.00087 https://doaj.org/article/aa8c515ecae848bc934c3b963bd83916 |