Modeling sediment movement in the shallow-water framework: A morpho-hydrodynamic approach with numerical simulations and experimental validation

被引:0
|
作者
Fernandez, E. Guerrero [1 ,2 ]
Diaz, M. J. Castro [3 ]
Wei, Y. [1 ,2 ]
Moore, C. [1 ]
机构
[1] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way NE Seattle, Seattle, WA 98115 USA
[2] Univ Washington, Cooperat Inst Climate Ocean & Ecosyst Studies, John M Wallace Hall,3737 Brooklyn Ave NE, Seattle, WA 98105 USA
[3] Univ Malaga, Fac Ciencias, Dept Anal Matemat, Campus Teatinos S-N, Malaga 29081, Spain
关键词
FINITE-VOLUME METHODS; HYDROSTATIC RECONSTRUCTION; HYPERBOLIC SYSTEMS; TRANSPORT MODELS; TSUNAMI DEPOSITS; SAND-TRANSPORT; EQUATIONS;
D O I
10.1016/j.ocemod.2024.102445
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This work presents a morpho-hydrodynamic model and a numerical approximation designed for the fast and accurate simulation of sediment movement associated with extreme events, such as tsunamis. The model integrates the well-established hydrostatic shallow-water equations with a transport equation for the moving bathymetry that relies on a bedload transport function. Subsequently, this model is discretized using the path-conservative finite volume framework to yield a numerical scheme that is not only fast but also second-order accurate and well-balanced for the lake-at-rest solution. The numerical discretization separates the hydrodynamic and morphodynamic components of the model but leverages the eigenstructure information to evolve the morphologic part in an upwind fashion, preventing spurious oscillations. The study includes various numerical experiments, incorporating comparisons with laboratory experimental data and field surveys.
引用
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页数:14
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