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Topographic Steering of Enhanced Ice Flow at the Bottleneck Between East and West Antarctica

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Authors:
  • Winter, Kate ;
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    Northumbria University
  • Ross, Neil ;
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    Newcastle University
  • Ferraccioli, Fausto ;
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    British Antarctic Survey
  • Jordan, Tom A. ;
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    British Antarctic Survey
  • Corr, Hugh F. J. ;
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    British Antarctic Survey
  • Forsberg, René ;
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    Orcid logo0000-0002-7288-9545
    National Space Institute, Technical University of Denmark
  • Matsuoka, Kenichi ;
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    Norwegian Polar Institute
  • Olesen, Arne V. ;
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    Orcid logo0000-0001-9555-9787
    National Space Institute, Technical University of Denmark
  • Casal, Tania G.
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    ESTEC
DOI:
10.1029/2018gl077504
Abstract:
Hypothesized drawdown of the East Antarctic Ice Sheet through the “bottleneck” zone between East and West Antarctica would have significant impacts for a large proportion of the Antarctic Ice Sheet. Earth observation satellite orbits and a sparseness of radio echo sounding data have restricted investigations of basal boundary controls on ice flow in this region until now. New airborne radio echo sounding surveys reveal complex topography of high relief beneath the southernmost Weddell/Ross ice divide, with three subglacial troughs connecting interior Antarctica to the Foundation and Patuxent Ice Streams and Siple Coast ice streams. These troughs route enhanced ice flow through the interior of Antarctica but limit potential drawdown of the East Antarctic Ice Sheet through the bottleneck zone. In a thinning or retreating scenario, these topographically controlled corridors of enhanced flow could however drive ice divide migration and increase mass discharge from interior West Antarctica to the Southern Ocean.
Type:
Journal article
Language:
English
Published in:
Geophysical Research Letters, 2018, Vol 45, Issue 10, p. 4899-4907
Main Research Area:
Science/technology
Publication Status:
Published
Review type:
Peer Review
Submission year:
2018
Scientific Level:
Scientific
ID:
2434266648

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