Destabilization of the Northeast Greenland Ice Stream

The Greenland Ice Sheet (GrIS) has been one of the largest contributors to global sea level rise over the last 20 years, accounting for c. 0.5 of a total of c. 3.2 mm yr-1. A significant portion of this contribution is associated with the speed up of glaciers in southeast and northwest Greenland. He...

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Bibliographic Details
Main Authors: Korsgaard, N. J., Khan, Shfaqat Abbas, Kjaer, K. H., Bevis, M. G., Bamber, J. L., Kjeldsen, K. K., Bjork, A. A., Wahr, J. M., Sterns, L. A., van den Broeke, M. R., Muresan, Ioana Stefania, Larsen, N. K.
Format: Conference Object
Language:English
Published: 2013
Subjects:
glacier
Greenland
Ice Sheet
Online Access:https://orbit.dtu.dk/en/publications/7bc98bdb-6b20-446b-af5a-a8ddb4df25be
https://backend.orbit.dtu.dk/ws/files/84768504/prod11389871184501.AGU6.pdf
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Summary:The Greenland Ice Sheet (GrIS) has been one of the largest contributors to global sea level rise over the last 20 years, accounting for c. 0.5 of a total of c. 3.2 mm yr-1. A significant portion of this contribution is associated with the speed up of glaciers in southeast and northwest Greenland. Here, we reveal that the Northeast Greenland Ice Stream (NEGIS), which extends more than 600 km into the interior of the ice sheet, is now undergoing dynamic thinning after more than a quarter of a century of stability. This sector of the GrIS is of particular interest in sea level projections, because the glacier flows into a large submarine basin with a negative bed slope near the grounding line. Our findings unfold the next step in mass loss of the GrIS as we show a heightened risk of rapid sustained loss from Northeast Greenland on top of the thinning in Southeast and Northwestern Greenland.

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