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            <title xml:lang="en">Tsunami generation by dynamic displacement of sea bed due to dip-slip faulting</title>
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            <funder>EU project TRANSFER (Tsunami Risk ANd Strategies For the European Region) of the sixth Framework Programme under contract no. 037058</funder>
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            <note type="commentary">22 pages, 10 figures, submitted to MATHEMATICS AND COMPUTERS IN SIMULATION. Other author's papers can be downloaded at http://www.cmla.ens-cachan.fr/~dutykh</note>
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                <title xml:lang="en">Tsunami generation by dynamic displacement of sea bed due to dip-slip faulting</title>
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                    <surname>Dias</surname>
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                <term xml:lang="en">seismic sources</term>
                <term xml:lang="en">tsunami</term>
                <term xml:lang="en">shallow water equations</term>
                <term xml:lang="en">finite volumes</term>
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              <p>In classical tsunami-generation techniques, one neglects the dynamic sea bed displacement resulting from fracturing of a seismic fault. The present study takes into account these dynamic effects. Earth's crust is assumed to be a Kelvin-Voigt material. The seismic source is assumed to be a dislocation in a viscoelastic medium. The fluid motion is described by the classical nonlinear shallow water equations (NSWE) with time-dependent bathymetry. The viscoelastodynamic equations are solved by a finite-element method and the NSWE by a finite-volume scheme. A comparison between static and dynamic tsunami-generation approaches is performed. The results of the numerical computations show differences between the two approaches and the dynamic effects could explain the complicated shapes of tsunami wave trains.</p>
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