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Abstract
This study analyzes a 35-year record of remotely sensed velocities and a 6-year record of repeated GPS observations at the East Greenland Ice-core Project (EastGRIP) to investigate ice flow acceleration in the Northeast Greenland Ice Stream (NEGIS). The findings reveal accelerating shear margins of NEGIS, indicating ice stream widening. Modeling suggests this widening is more consistent with shear margin softening (due to fabric evolution or temperature changes) than external forcing at the surface or bed, despite recent large dynamical changes at NEGIS outlets.
Publisher
Nature Communications
Published On
Sep 23, 2022
Authors
Aslak Grinsted, Christine S. Hvidberg, David A. Lilien, Nicholas M. Rathmann, Nanna B. Karlsson, Tamara Gerber, Helle Astrid Kjær, Paul Vallelonga, Dorthe Dahl-Jensen
Tags
ice flow
Greenland Ice Stream
Northeast Greenland Ice Stream
shear margins
acceleration
fabric evolution
temperature changes
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