U.S. Dept. of Commerce / NOAA / OAR / PMEL
The Global Reach of the 26 December 2004 Sumatra Tsunami
V. Titov,1 A. B. Rabinovich,2,3 H. O. Mofjeld,1 R. E. Thomson,2 and F. I. González1
1NOAA/Pacific Marine Environmental Laboratory, Seattle, Washington
2Institute of Ocean Sciences, Department of Fisheries and Oceans Canada, Sidney, British Columbia, Canada
3P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Science, 309(5743), 2045–2048, 2005.
Copyright ©2005 by The American Association for the Advancement of Science. Further electronic distribution
is not allowed.
Numerical model simulations, combined with tide-gauge and satellite altimetry data, reveal that wave amplitudes, directionality, and global propagation patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orientation and intensity of the offshore seismic line source and subsequently by the trapping effect of mid-ocean ridge topographic waveguides.
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