Surface Melt-Induced Acceleration of Greenland Ice-Sheet Flow

Ice flow at a location in the equilibrium zone of the west-central Greenland Ice Sheet accelerates above the midwinter average rate during periods of summer melting. The near coincidence of the ice acceleration with the duration of surface melting, followed by deceleration after the melting ceases,...

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Bibliographic Details
Published in:Science
Main Authors: Zwally, H. Jay, Abdalati, Waleed, Herring, Tom, Larson, Kristine, Saba, Jack, Steffen, Konrad
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2002
Subjects:
Online Access:http://dx.doi.org/10.1126/science.1072708
https://www.science.org/doi/pdf/10.1126/science.1072708