Despite this progress approximation of, a tsunami
source as a, point source i.e. Epicenter, plus magnitude is usually
insufficient. For reliable near-field tsunami early warning
since, for large subduction events happening not far from the
coast rupture,, Propagation direction and source extent cannot
be neglected (Babeyko et al, 2010). Buoys together with
.Ocean bottom sensors help to gain additional source information
in case of, transoceanic tsunamis but would not be
effective. In the near-field due to time constraints.
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