Englacial Warming Indicates Deep Crevassing in Bowdoin Glacier, Greenland

All around the margins of the Greenland Ice Sheet, marine-terminating glaciers have recently thinned and accelerated. The reduced basal friction has yielded increased flow velocity, while the rate of longitudinal stretching has been limited by ice viscosity, which itself critically depends on temper...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Seguinot, Julien, Funk, Martin, Bauder, Andreas, Wyder, Thomas, Senn, Cornelius, Sugiyama, Shin
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media
Subjects:
450
Online Access:http://hdl.handle.net/2115/78127
https://doi.org/10.3389/feart.2020.00065