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We present a highly accurate and computationally efficient method (herein,the "wavefront orientation method") for determining the travel time ofoceanic tsunamis. Based on Huygens' Principle, the method uses an eight-pointgrid-point pattern and the most recent information on the orientation of theadvancing wavefront to determine the time for a tsunami to travel to aspecific oceanic location. The method is shown to provide improved accuracyand reduced anisotropy compared with the conventional multiple grid-pointmethod presently in widespread use

A wavefront orientation method for precise numerical determination of tsunami travel time