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Effect of the Bottom Topography on Tsunami Propagation in the East (Japan) Sea
引用本文:CHOI Byung-Ho,;PELINOVSKY Efim,;JEON Chul-Kyoo,;KIM Kyeong-Ok. Effect of the Bottom Topography on Tsunami Propagation in the East (Japan) Sea[J]. 中国海洋工程, 2008, 22(2): 277-290
作者姓名:CHOI Byung-Ho,  PELINOVSKY Efim,  JEON Chul-Kyoo,  KIM Kyeong-Ok
作者单位:Department of Civil and Environmental Engineering Sungkyunkwan University,Department of Nonlinear Geophysical Processes Institute of Applied Physics,Nizhny Novgorod 603950 Russia,Department of Civil and Environmental Engineering Sungkyunkwan University,Department of Civil and Environmental Engineering Sungkyunkwan University,Suwon 440-746 Korea,Suwon 440-746 Korea,Suwon 440-746 Korea
基金项目:The work was financially supported by the Korean Ministry of Land, Transport and Maritime Affairs, and INTAS (Grant No. 06-1000013-9236)
摘    要:A study of tsunami events in the East (Japan) Sea using continuous Galerkin finite element model, aiming at reproducing tsunami waves generated by underwater earthquakes in 1983 and 1993 respectively has been performed focusing on the geographic extent of a topographic feature in the East (Japan) Sea. Numerical models can be the proper tools to study the combined effects of realistic topography. Subsequently, using the FEM based two-dimensional model we have simulated the smoothed and flattened topographic effects by removal of Yamato Rise and seamounts for the cases of tthe 1983 Central region earthquake tsunami and the 1993 southwestern Hokkaido earthquake tsunami. The results have shown that there will be higher tsunamis along the eastern coasts of Korea in general except some areas, like Sokcho with removal of topographic highs, thus providing complicated bottom topography of the East (Japan) Sea as effective tsunami energy scattering.

关 键 词:日本  海隆  海啸  海底地形学

Effect of the Bottom Topography on Tsunami Propagation in the East (Japan) Sea
CHOI Byung-Ho,PELINOVSKY Efim,JEON Chul-Kyoo,KIM Kyeong-Ok. Effect of the Bottom Topography on Tsunami Propagation in the East (Japan) Sea[J]. China Ocean Engineering, 2008, 22(2): 277-290
Authors:CHOI Byung-Ho  PELINOVSKY Efim  JEON Chul-Kyoo  KIM Kyeong-Ok
Affiliation:[1]Department of Civil and Environmental Engineering, Sungkyunkucan University, Suwon 440-746, Korea [2]Department of Nonlinear Geophysical Processes, Institute of Applied Physics, Nizhny Novgorod 603950, Russia
Abstract:A study of tsunami events in the East (Japan) Sea using continuous Galerkin finite element model, aiming at reproducing tsunami waves generated by underwater earthquakes in 1983 and 1993 respectively has been performed focusing on the geographic extent of a topographic feature in the East (Japan) Sea. Numerical models can be the proper tools to study the combined effects of realistic topography. Subsequently, using the FEM based two-dimensional model we have simulated the smoothed and flattened topographic effects by removal of Yamato Rise and seamounts for the cases of tthe 1983 Central region earthquake tsunami and the 1993 southwestern Hokkaido earthquake tsunami. The results have shown that there will be higher tsunamis along the eastern coasts of Korea in general except some areas, like Sokcho with removal of topographic highs, thus providing complicated bottom topography of the East (Japan) Sea as effective tsunami energy scattering.
Keywords:Yamato Rise  1983 central East (Japan) Sea tsunami  1993 southwestern Hokkaido tsunami
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