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...
Published in: | Geological Society, London, Memoirs |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Digital Commons @ University of South Florida
2016
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Subjects: | |
Online Access: | https://digitalcommons.usf.edu/msc_facpub/1562 https://doi.org/10.1144/M46.173 |