Nonlinear interaction between ocean tides and the Larsen C Ice Shelf system
Author:
Affiliation:
1. School of Civil Engineering and Geosciences; Newcastle University; Newcastle upon Tyne UK
2. British Antarctic Survey; Cambridge UK
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1108/2011GL046680/2011GL046680.pdf
Reference20 articles.
1. Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf;Anandakrishnan;Geophys. Res. Lett.,2003
2. Till beneath Ice Stream B: 1. Properties derived from seismic travel times;Blankenship;J. Geophys. Res.,1987
3. Flow of the Ross Ice Shelf, Antarctica, is modulated by the ocean tide;Brunt;J. Glaciol.,2010
4. Tide-induced lateral movement of Brunt Ice Shelf, Antarctica;Doake;Geophys. Res. Lett.,2002
5. Surface structure and stability of the Larsen C ice shelf, Antarctic Peninsula;Glasser;J. Glaciol.,2009
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