RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES4004, doi:10.2205/2006ES000214, 2006

2006ES000214-fig02.html
Figure 2. (a) Altimetry sea-level taken along track 129 of the Jason-1 satellite for Cycle 109 and along the same track 10 days earlier for Cycle 108; and (b) wavelet analysis of the sea level profile in (a). The solid line is the theoretical dispersion curve derived using equation (3). The vertical dashed line marks the boundary of the "wave affected" area associated with a seismotectonic source having spatial coverage scale Lapprox T (gH)1/2 (for T = 2 hours). To the north of this boundary is a "wave void region" into which no waves have propagated. Letter "T" indicates the tsunami wavefront.

RJES

Citation: Kulikov, E. (2006), Dispersion of the Sumatra Tsunami waves in the Indian Ocean detected by satellite altimetry, Russ. J. Earth Sci., 8, ES4004, doi:10.2205/2006ES000214.

Copyright 2006 by the Russian Journal of Earth Sciences
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