Tide-induced lateral movement of Brunt Ice Shelf, Antarctica

[1] Accurate position data show that Brunt Ice Shelf has an irregular three-dimensional motion driven by the ocean tide. A 30-day GPS record from Halley station shows not only the expected vertical tidal displacement, but also a significant variation in horizontal velocity. The maximum forward veloc...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Doake, C.S.M., Corr, H.F.J., Nicholls, K.W., Gaffikin, A., Jenkins, A., Bertiger, W.I., King, M.A.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2002
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/13264/
http://www.agu.org/journals/gl/gl0208/2001GL014606/2001GL014606.pdf