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海啸在冲绳海槽和东海浅水大陆架地形上产生和传播的数值模拟
引用本文:李伟,朱元清,王本龙,宋治平.海啸在冲绳海槽和东海浅水大陆架地形上产生和传播的数值模拟[J].地震地磁观测与研究,2007,28(5):138-142.
作者姓名:李伟  朱元清  王本龙  宋治平
作者单位:1. 中国上海,200062,上海市地震局
2. 中国上海,200240,上海交通大学
摘    要:运用数值模拟的方法对在冲绳海槽产生9.0级地震,并引发海啸的过程和海啸波在东海浅水大陆架地形上的传播过程进行研究.模拟的结果表明,数值模拟产生的波浪符合海啸波的特点,东海浅水大陆架适合海啸波的传播.

关 键 词:海啸  数值模拟  高阶Boussinesq方程  浅水大陆架
文章编号:1003-3246(2007)05-0138-05

The numerical simulation of tsunamis wave on Okinawa Trough and continental shelf of the East China Sea
Li Wei,Zhu Yuanqing,Wang Benlong,Song Zhiping.The numerical simulation of tsunamis wave on Okinawa Trough and continental shelf of the East China Sea[J].Seismological and Geomagnetic Observation and Research,2007,28(5):138-142.
Authors:Li Wei  Zhu Yuanqing  Wang Benlong  Song Zhiping
Institution:1Earthquake Administration of Shanghai Municipality, Shanghai 200062,China ;2.Shanghai J iaotong University, Shanghai 200240, China
Abstract:Using the method of numerical simulation, we computed the movement track of tsunamis wave which was engendered by Ms 9.0 large earthquake in Okinawa Trough. Features of landform structure of the continental shelf of the East China Sea were analyzed. We indicated that tsunamis wave simulated could propagate on continental shelf of the East China Sea and accord with characters of actual tsunamis wave.
Keywords:tsunamis  numerical simulation  higher order Boussinesq model  continental shelf shallow-water area
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