Flow variability and ongoing margin shifts on Bindschadler and MacAyeal Ice Streams, West Antarctica
Author:
Affiliation:
1. National School of Surveying; University of Otago; Dunedin New Zealand
2. US National Snow and Ice Data Center; University of Colorado Boulder; Boulder Colorado USA
3. Geophysical Institute; University of Alaska; Fairbanks Alaska USA
Funder
New Zealand Antarctic Research Institute
Publisher
American Geophysical Union (AGU)
Subject
Earth-Surface Processes,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JF003670/fullpdf
Reference46 articles.
1. Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf;Anandakrishnan;Geophys. Res. Lett.,2003
2. Onset of streaming flow in the Siple Coast region, West Antarctica;Bindschadler;Antarct. Res. Ser.,2001
3. Surface velocity and mass balance of ice streams D and E, West Antarctica;Bindschadler;J. Glaciol.,1996
4. Tidally controlled stick-slip discharge of a West Antarctic ice stream;Bindschadler;Science,2003
5. Numerical investigations of the slow-down of Whillans Ice Stream, West Antarctica: Is it shutting down like Ice Stream C?;Bougamont;Ann. Glaciol.,2003
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