Sustained retreat of the Pine Island Glacier

We use satellite observations to show that, between 1992 and 2011, the Pine Island Glacier hinge line retreated at a rate of 0.95 ± 0.09 km yr−1 despite a progressive steepening and shoaling of the glacier surface and bedrock slopes, respectively, which ought to impede retreat. The retreat has remai...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Park, J. W., Gourmelen, N., Shepherd, A., Kim, S. W., Vaughan, D. G., Wingham, D. J.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2013
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/502339/
https://nora.nerc.ac.uk/id/eprint/502339/1/grl50379.pdf
https://doi.org/10.1002/grl.50379