Rapid grounding line migration induced by internal ice stream variability
Author:
Affiliation:
1. Department of Earth and Planetary Sciences; Harvard University; Cambridge Massachusetts USA
2. Department of Earth and Ocean Sciences; University of British Columbia; Vancouver British Columbia Canada
Funder
NSF
NSF Graduate Research Fellowship
NSERC Discovery
Publisher
American Geophysical Union (AGU)
Subject
Earth-Surface Processes,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JF003251/fullpdf
Reference73 articles.
1. Deformation of till beneath ice stream B, West Antarctica;Alley;Nature,1986
2. Discovery of till deposition at the grounding line of Whillans Ice Stream;Anandakrishnan;Science,2007
3. Widespread complex flow in the interior of the Antarctic ice sheet;Bamber;Science,2000
4. Ice streams as the arteries of an ice sheet: Their mechanics, stability and significance;Bennett;Earth Sci. Rev.,2003
5. Seismic measurements reveal a saturated porous layer beneath an active Antarctic ice stream;Blankenship;Nature,1986
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