| NONLINEAR NUMERICAL COMPUTATIONS ON STORM SURGES OF THE TAIWAN STRAIT |
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| 作者姓名： | 吴培木 许永水 李燕初 陈玉霞 陈季良 |
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| 作者单位： | Third Institute of Oceanography，National Bureau of Oceanography，Xiamen，Third Institute of Oceanography，National Bureau of Oceanography，Xiamen，Third Institute of Oceanography，National Bureau of Oceanography，Xiamen，Third Institute of Oceanography，National Bureau of Oceanography，Xiamen，Third Institute of Oceanography，National Bureau of Oceanography，Xiamen |
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| 摘 要： | In order to make up well a complete picture of storm surges in the area of theTaiwan Strait, to find out and further study the formation mechanism and regularity ofstorm surges of this strait, nonlinear numerical computations have been made on thestorm surges formed by typhoon which directly hit the area along three main tracks. Inaccordance with the current field of shallow-sea storm surges with the characteristics of"boundary layer" current field, the finite difference technique is adopted on the basis ofthe whole current equations of storm surges, and the anticipated results are obtained.
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| 收稿时间： | 1/3/1980 12:00:00 AM |
NONLINEAR NUMERICAL COMPUTATIONS ON STORM SURGES OF THE TAIWAN STRAIT |
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| WU PEIMU,XU YONGSHUI,LI YANCHU,CHEN YUXIA and CHEN JILIANG.NONLINEAR NUMERICAL COMPUTATIONS ON STORM SURGES OF THE TAIWAN STRAIT[J].Acta Oceanologica Sinica,1982,1(2):195-203. |
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| Authors: | WU PEIMU XU YONGSHUI LI YANCHU CHEN YUXIA and CHEN JILIANG |
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| Institution: | Third Institute of Oceanography, National Bureau of Oceanography, Xiamen |
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| Abstract: | In order to make up well a complete picture of storm surges in the area of theTaiwan Strait,to find out and further study the formation mechanism and regularity ofstorm surges of this strait,nonlinear numerical computations have been made on thestorm surges formed by typhoon which directly hit the area along three main tracks.Inaccordance with the current field of shallow-sea storm surges with the characteristics of "boundary layer" current field,the finite difference technique is adopted on the basis ofthe whole current equations of storm surges,and the anticipated results are obtained. |
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