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Tsunami generation by dynamic displacement of sea bed due to dip-slip faulting

Abstract : 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.
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https://hal.archives-ouvertes.fr/hal-00174439
Contributor : Denys Dutykh <>
Submitted on : Friday, June 6, 2008 - 9:43:43 AM
Last modification on : Thursday, July 2, 2020 - 5:17:18 PM
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Denys Dutykh, Frédéric Dias. Tsunami generation by dynamic displacement of sea bed due to dip-slip faulting. Mathematics and Computers in Simulation, Elsevier, 2009, Mathematics and Computers in Simulation, 80 (4), pp.837-848. ⟨10.1016/j.matcom.2009.08.036⟩. ⟨hal-00174439v3⟩

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