wei shi li lun he xiang fang fa zai feng hai liu yu sheng jiang liu yan jiu zhong de ying yong
Author(s): LI XIN-MING AND WANG JING-YONG
Pages: 94-112
Year: 1965 Issue: 2
Journal: Oceanologia et Limnologia Sinica
Keyword: 风海流; 升降流; 位势理论; 象方; 水平流; 海岸; 有限深度; 风系; 研究中; 海域;
Abstract: So far, the method of Fourier transform has been most frequently employed in the ocean current studies. In the present paper the potential theory and the method of image are introduced in the discussions of ocean currents. The proposed methods proved to be better; they solved in terms of special functions the space problem of drift and up-welling currents in the cases of both infinite and finite depths, solutions to the latter case being obtained for the first time. Numerical calculations are given for coastal currents in the case of infinite depth, the results being satisfactory as compared with that of K. Hidaka's theory and in agreement with Saito's result.
Pages: 94-112
Year: 1965 Issue: 2
Journal: Oceanologia et Limnologia Sinica
Keyword: 风海流; 升降流; 位势理论; 象方; 水平流; 海岸; 有限深度; 风系; 研究中; 海域;
Abstract: So far, the method of Fourier transform has been most frequently employed in the ocean current studies. In the present paper the potential theory and the method of image are introduced in the discussions of ocean currents. The proposed methods proved to be better; they solved in terms of special functions the space problem of drift and up-welling currents in the cases of both infinite and finite depths, solutions to the latter case being obtained for the first time. Numerical calculations are given for coastal currents in the case of infinite depth, the results being satisfactory as compared with that of K. Hidaka's theory and in agreement with Saito's result.
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