Submarine glacial landform distribution across the West Antarctic margin, from grounding line to slope: the Pine Island-Thwaites ice stream system
About 30% of ice draining the West Antarctic Ice Sheet discharges through several glacier systems into the Amundsen Sea Embayment (ASE) (Fig. 1a). Two major ice-stream outlets, Pine Island and Thwaites glaciers, have undergone significant twentieth century changes (e.g. Rignot et al. 2008) and much...
Main Authors: | , , , , , , , , , |
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Other Authors: | , , , , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society of London
2016
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/513836/ http://mem.lyellcollection.org/content/46/1/493.short |