Subglacial melt channels and fracture in the floating part of Pine Island Glacier, Antarctica

A dense grid of ice-penetrating radar sections acquired over Pine Island Glacier, West Antarctica has revealed a network of sinuous subglacial channels, typically 500 m to 3 km wide, and up to 200 m high, in the ice-shelf base. These subglacial channels develop while the ice is floating and result f...

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Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Vaughan, David G., Corr, Hugh F. J., Bindschadler, Robert A., Dutrieux, Pierre, Gudmundsson, G. Hilmar, Jenkins, Adrian, Newman, Thomas, Vornberger, Patricia, Wingham, Duncan J.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2012
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/19568/
https://nora.nerc.ac.uk/id/eprint/19568/1/2012JF002360.pdf
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2012JF002360