Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf
Author:
Affiliation:
1. Earth and Mineral Sciences Environment Institute, Department of Geosciences; Pennsylvania State University; University Park Pennsylvania USA
2. School of Civil Engineering and Geosciences; University of Newcastle Upon Tyne; Newcastle Upon Tyne UK
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Reference23 articles.
1. Tidal forcing of basal seismicity of ice stream C, West Antarctica, observed far inland;Anandakrishnan;J. Geophys. Res.,1997
2. Diurnal stick-slip motion in the mouth of Whillans Ice Stream;Bindschadler;Ann. Glaciol,2003
3. Response of well-aquifer systems to Earth tides;Bredehoeft;J. Geophys. Res.,1967
4. Glaciological studies on Rutford Ice Stream, Antarctica;Doake;J. Geophys. Res.,1987
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