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Patrick J. Lynett

Researcher at University of Southern California

Publications -  158
Citations -  4900

Patrick J. Lynett is an academic researcher from University of Southern California. The author has contributed to research in topics: Nonlinear system & Landslide. The author has an hindex of 35, co-authored 151 publications receiving 4230 citations. Previous affiliations of Patrick J. Lynett include Cornell University & Northwestern University.

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Laboratory and numerical studies of wave damping by emergent and near-emergent wetland vegetation

TL;DR: In this article, the authors measured wave attenuation resulting from synthetic emergent and nearly emergent wetland vegetation under a range of wave conditions and plant stem densities using linear wave theory to quantify bulk drag coefficients and with a nonlinear Boussinesq model to determine numerical friction factors.
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Modeling wave runup with depth-integrated equations

TL;DR: In this paper, a moving boundary technique was developed to investigate wave runup and rundown with depth-integrated equations using a high-order finite difference scheme, which is used to solve highly nonlinear and weakly dispersive equations.
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Observations by the International Tsunami Survey Team in Sri Lanka

TL;DR: The conclusion stresses the importance of education: Residents with a basic knowledge of tsunamis, as well as an understanding of how environmental modifications will affect overland flow, are paramount to saving lives and minimizing tsunami destruction.
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A numerical study of submarine-landslide-generated waves and run-up

TL;DR: In this paper, a mathematical model is derived to describe the generation and propagation of water waves by a submarine landslide, which consists of a depth-integrated continuity equation and momentum equations, in which the ground movement is the forcing function.
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A two-layer approach to wave modelling

TL;DR: In this article, a set of model equations for water wave propagation is derived by piecewise integration of the primitive equations of motion through two arbitrary layers and an independent velocity profile is derived.