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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
2002
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/13264/ http://www.agu.org/journals/gl/gl0208/2001GL014606/2001GL014606.pdf |