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Jeffrey C. Harris

Researcher at École Normale Supérieure

Publications -  33
Citations -  1502

Jeffrey C. Harris is an academic researcher from École Normale Supérieure. The author has contributed to research in topics: Nonlinear system & Potential flow. The author has an hindex of 12, co-authored 31 publications receiving 1285 citations. Previous affiliations of Jeffrey C. Harris include University of Rhode Island & University of Paris.

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A high-order adaptive time-stepping TVD solver for Boussinesq modeling of breaking waves and coastal inundation

TL;DR: A high-order adaptive time-stepping TVD solver for the fully nonlinear Boussinesq model of Chen (2006), extended to include moving reference level as in Kennedy et al. (2001).
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Did a submarine landslide contribute to the 2011 Tohoku tsunami

TL;DR: In this article, an analysis of seismic and geodetic data, together with recorded tsunami waveforms, was performed to infer the location of the most likely additional source of the 2011 Tohoku tsunami from a submarine mass failure (SMF).
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Numerical Simulation of the 2011 Tohoku Tsunami Based on a New Transient FEM Co-seismic Source: Comparison to Far- and Near-Field Observations

TL;DR: In this article, the authors simulate the 2011 Tohoku-Oki tsunami using new coseismic tsunami sources based on inverting onshore and offshore geodetic data, using 3D Finite Element Models (FEMs).
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Dispersive tsunami waves in the ocean: Model equations and sensitivity to dispersion and Coriolis effects

TL;DR: In this paper, the authors derived fully nonlinear, weakly dispersive model equations for propagation of surface gravity waves in a shallow, homogeneous ocean of variable depth on the surface of a rotating sphere.
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Numerical modeling of tsunami waves generated by the flank collapse of the Cumbre Vieja Volcano (La Palma, Canary Islands): Tsunami source and near field effects

TL;DR: In this article, the authors studied the wave propagation in the case of the collapse of the Cumbre Vieja Volcano (CVV) in the Canary Island of Spain using a 3D Navier-Stokes model and 2D Boussinesq model.