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

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
L
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.

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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