Ice‐flow structure and ice dynamic changes in the Weddell Sea sector of West Antarctica from radar‐imaged internal layering-Reference-Cited by-同舟云学术

Ice‐flow structure and ice dynamic changes in the Weddell Sea sector of West Antarctica from radar‐imaged internal layering

Published:2015-04 Issue:4 Volume:120 Page:655-670
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Bingham Robert G.¹^ORCID,Rippin David M.²,Karlsson Nanna B.³,Corr Hugh F. J.⁴,Ferraccioli Fausto⁴,Jordan Tom A.⁴,Le Brocq Anne M.⁵,Rose Kathryn C.⁶,Ross Neil⁷,Siegert Martin J.⁸

Affiliation:

1. School of GeoSciences University of Edinburgh Edinburgh UK

2. Environment Department University of York York UK

3. Centre for Ice and Climate Niels Bohr Institute, University of Copenhagen Copenhagen Denmark

4. British Antarctic Survey Natural Environment Research Council Cambridge UK

5. Geography, College of Life and Environmental Sciences University of Exeter Exeter UK

6. Bristol Glaciology Centre, School of Geographical Sciences University of Bristol Bristol UK

7. School of Geography, Politics and Sociology Newcastle University Newcastle UK

8. Grantham Institute and Department of Earth Science and Engineering Imperial College London London UK

Funder

NERC Antarctic Funding Initiative

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014JF003291

Reference67 articles.

1. Influence of subglacial geology on the position of a West Antarctic ice stream from seismic observations

2. Widespread Persistent Thickening of the East Antarctic Ice Sheet by Freezing from the Base

3. Deglacial history of the West Antarctic Ice Sheet in the Weddell Sea embayment: Constraints on past ice volume change

4. Getting around Antarctica: new high-resolution mappings of the grounded and freely-floating boundaries of the Antarctic ice sheet created for the International Polar Year

5. Radar-derived bed roughness characterization of Institute and Möller ice streams, West Antarctica, and comparison with Siple Coast ice streams

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