2019
DOI: 10.1016/j.cageo.2019.06.010
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Numerical study of tsunami wave run-up and land inundation on coastal vegetated beaches

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Cited by 20 publications
(4 citation statements)
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“…The physical variables are the same in every triangular mesh element because of the average depth integration in the equation; a series of piecewise functions are developed in the solution domain. The approach of the Monotonic Upstream-Centered Scheme for Conservation Laws with a multi-dimensional limiter and the Roe's approximate Riemann solver were used to calculate the interface fluxes between triangular grid cells [32][33].…”
Section: Hydrodynamic Modelmentioning
confidence: 99%
“…The physical variables are the same in every triangular mesh element because of the average depth integration in the equation; a series of piecewise functions are developed in the solution domain. The approach of the Monotonic Upstream-Centered Scheme for Conservation Laws with a multi-dimensional limiter and the Roe's approximate Riemann solver were used to calculate the interface fluxes between triangular grid cells [32][33].…”
Section: Hydrodynamic Modelmentioning
confidence: 99%
“…For instance, by applying an improved Boussunesq wave model, the wave attenuation properties of flexible and rigid vegetation patches were systematically analyzed by Augustin et al [45] and Huang et al [22]. In addition, the hydrodynamic processes of ocean surface waves in the vegetation patches were also numerically simulated by applying the shallow water equations [46][47][48]. Nevertheless, the complex flow field within the wave-vegetation interactions often contains strong vertical accelerations, which beyond the computational capability of the Boussinesq wave model and the nonlinear shallow water models [49].…”
Section: Introductionmentioning
confidence: 99%
“…But as the waves travel onshore, they increase in height as the bathymetry gradually decrease, becoming potentially destructive (e.g., the tsunami in Indian Ocean in December 2004, or in Japan in March 2011). Usually the tsunami were modelled as solitary waves and obliviously the shoaling, breaking, and run-up are phenoma of major interest for researcher [4][5][6][7][8][9]. The high computational power of modern computers and parallel computing make it possible to solve more and more complex fluid dynamics problems.…”
Section: Introductionmentioning
confidence: 99%