Steep reverse bed slope at the grounding line of the Weddell Sea sector in West Antarctica

The bed of the West Antarctic Ice Sheet is, in places, more than 1.5 km below sea level1, 2. It has been suggested that a positive ice-loss feedback may occur when an ice sheet’s grounding line retreats across a deepening bed1, 2, 3. Applied to the West Antarctic Ice Sheet, this process could potent...

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Bibliographic Details
Published in:Nature Geoscience
Main Authors: Ross, Neil, Bingham, Robert G., Corr, Hugh F.J., Ferraccioli, Fausto, Jordan, Tom, Le Brocq, Anne, Rippin, David M., Young, Duncan, Blakenship, Donald D., Siegert, Martin J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2012
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/18012/