Uppermost crustal structure regulates the flow of the Greenland Ice Sheet

The flow of the Greenland Ice Sheet is controlled by subglacial processes and conditions that depend on the geological provenance and temperature of the crust beneath it, neither of which are adequately known. Here we present a seismic velocity model of the uppermost 5 km of the Greenlandic crust. W...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Jones, G. A., Ferreira, A. M. G., Kulessa, B., Schimmel, M., Berbellini, A., Morelli, A.
Format: Text
Language:English
Published: Nature Publishing Group UK 2021
Subjects:
Article
Greenland
glacier
greenlandic
Ice Sheet
Iceland
Jakobshavn
Petermann glacier
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8674248/
http://www.ncbi.nlm.nih.gov/pubmed/34911961
https://doi.org/10.1038/s41467-021-27537-5
Description
Summary:The flow of the Greenland Ice Sheet is controlled by subglacial processes and conditions that depend on the geological provenance and temperature of the crust beneath it, neither of which are adequately known. Here we present a seismic velocity model of the uppermost 5 km of the Greenlandic crust. We show that slow velocities in the upper crust tend to be associated with major outlet glaciers along the ice-sheet margin, and elevated geothermal heat flux along the Iceland hotspot track inland. Outlet glaciers particularly susceptible to basal slip over deformable subglacial sediments include Jakobshavn, Helheim and Kangerdlussuaq, while geothermal warming and softening of basal ice may affect the onset of faster ice flow at Petermann Glacier and the Northeast Greenland Ice Stream. Interactions with the solid earth therefore control the past, present and future dynamics of the Greenland Ice Sheet and must be adequately explored and implemented in ice sheet models.

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