Modeling Tsunami in South China Sea with Boussinesq equations

被引:4
|
作者
Ren, Zhiyuan [1 ]
Liu, Hua [1 ]
机构
[1] Shanghai Jiao Tong Univ, MOE Key Lab Hydrodynam, Sch NAOCE, Shanghai 200240, Peoples R China
关键词
Tsunami; South China Sea; Boussinesq equations; Manila Trench; DISPERSION; PROPAGATION;
D O I
10.1016/j.proeng.2015.08.378
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
To describe the dispersion effects, the high order Boussinesq (FUNWAVE) is adopted to simulate the tsunami propagating from Manila Trench to the South China Sea region. The Okada model is employed to generate tsunami, the surface elevation and depth-averaged horizontal velocity at t=5 min computed by the shallow water equations are then interpolated to serve as the initial condition of the Boussinesq model. Different tsunami propagation scenarios with magnitude of M-w=8.0 are presented, and the arrival time and tsunami wave distribution are described and analyzed for the assessment of tsunami hazard near coasts around South China Sea. It is concluded that the dispersion effects in South China Sea is not significant. (C) 2015 Published by Elsevier Ltd.
引用
收藏
页码:888 / 896
页数:9
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