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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS002 Poster presentation 1793<br />

Modeling of the UHF Radar signature of a tsunami approaching coastal<br />

areas: application to tsunami warning<br />

Prof. Stephan Grilli<br />

Department of Ocean Engineering University of Rhode Island<br />

Marc Saillard, Sara Dubosq<br />

During the catastrophic 12/26/04 tsunami, perhaps for the first time, satellite remote sensing (radar<br />

altimetry) was able to provide transects of tsunami elevation across the Indian Ocean while the event<br />

unfolded (e.g., Jason I). Here we similarly use well established Ultra High Frequency (UHF) radar<br />

technology, to develop a method that could provide warning of an incoming tsunami to coastal<br />

populations. When a tsunami reaches the continental shelf, the mostly depth-uniform current it induces,<br />

indeed greatly increases in speed (maybe up to 10-20 cm/s) and starts causing significant Doppler shifts<br />

in ocean surface waves, particularly those of smaller wavelength (high frequency). Such shifts may be<br />

recognized as a typical signature, by a shore-based UHF radar, and thus trigger a warning, provided<br />

proper numerical simulations and sensitivity analyses have been performed ahead of time. Since<br />

tsunamis very much slow down due to decreasing water depth, from the shelf break to shore, warning<br />

times 5-15 minutes could be conceivable, depending on the shelf width. Here, we use a Higher Order<br />

Spectral (HOS) Method to model fully nonlinear sea states caused by wind, down to typical UHF<br />

wavelength of order 10 cm, as well as Doppler shifts and wave shoaling and refraction caused by a<br />

slowly varying depth uniform current. The latter current is obtained from tsunami propagation modeling,<br />

using a standard long wave model, for some selected case studies. UHF radar backscattering is modeled<br />

by a Boundary Element Method solving Maxwells equations, developed and validated in earlier work. We<br />

present initial results of this modeling study, in terms of spatio-temporal UHF radar signatures<br />

corresponding to some tsunami case studies. In particular, we apply this methodology to southern<br />

Thailand, based on earlier modeling work we performed for tsunami runup caused in Thailand for the<br />

12/26/04 tsunami.<br />

Keywords: tsunam modeling, remote sensing, warning systems

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