东海南部陆架对半日分潮波的增大效应
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摘要: 浙江沿岸是我国潮差分布最大的地带,其原因之一是相邻接的陆架对半日潮波的增大效应.本文引用一种模型论述其可能发生的原因.理论上分析得出,半日分潮在这一海域存在发生共振的条件,而全日分潮则否;结合比较接近真实陆架地形的分析表明,沿岸半日分潮(M2)的振幅比陆架外缘大约增大4倍,这与实测结果基本一致.
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Fleeting,R,H.,Tides and tidal cur.-eats iz the Gulf of Panana,Journal of hlerine Research,1(1938),3:192-266. Redfield,A,C.,The influence of the continental shelf on the tides of the Atlantic coast of the United States,Journal of ATarias Research,17(1958),432-448. Munk,W,et al.,Tides offshore:transition froet California coastal to deep-sea waters,Geophysical Fluid Dynamics,1(1970)2.161-235. Miles,J.W.,Kelvin waves on oceanic boundaries,Journal of Fluid Mechanics,55(1972),1:113-127. Clarke,A.J,and D,S,Battisti,The effect of continental shelves on tides,Deep-Sea Research,A28(1981).7:665-682. 林美华,东海海底地形的特征,海洋科学,5(1981),1:24-27. Fang Guohong,Tides and tidal currents in the n arginal seas adjacent to China,J,Oceanol,Limnol.,4(1986),1:1-16. 陈宗墉,潮汐学.科学出版社,1981,76. -
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