Tide-induced lateral movement of Brunt Ice Shelf, Antarctica-Reference-Cited by-同舟云学术

Tide-induced lateral movement of Brunt Ice Shelf, Antarctica

Published:2002-04 Issue:8 Volume:29 Page:67-1-67-4
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Doake C. S. M.¹,Corr H. F. J.¹,Nicholls K. W.¹,Gaffikin A.¹,Jenkins A.¹,Bertiger W. I.²,King M. A.³

Affiliation:

1. British Antarctic Survey; Natural Environment Research Council; Cambridge UK

2. Jet Propulsion Laboratory; California Institute of Technology; Pasadena USA

3. Department of Geomatics; University of Newcastle; Newcastle upon Tyne UK

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference17 articles.

1. Tidal forcing of basal seismicity of ice stream C, West Antarctica, observed far inland;Anandakrishnan;Journal of Geophysical Research,1997

2. Anandakrishnan , S. J. C. Bowling R. B. Alley D. E. Voigt The flow velocity of the ice plain of ice stream D is modulated by the ocean tide Sterling, Virginia, USA 2001

3. Recent glaciological investigations on Brunt Ice Shelf;Doake;Filchner Ronne Ice Shelf Programme,2000

4. Treatment of horizontal and vertical tidal signals in GPS data: A case study on a floating ice shelf;King;Earth Planets & Space,2000

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