Tide-induced lateral movement of Brunt Ice Shelf, Antarctica

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 velocity...

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Veröffentlicht in:	Geophysical research letters 2002-04, Vol.29 (8), p.67-1-67-4
Hauptverfasser:	Doake, C. S. M., Corr, H. F. J., Nicholls, K. W., Gaffikin, A., Jenkins, A., Bertiger, W. I., King, M. A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Friction Horizontal Oceans Permissible error Phase relationships Shelves Stations Synthetic aperture radar
Online-Zugang:	Volltext
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