长江口外的上升流现象
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摘要: 我国近海的上升流现象已经引起人们的浓厚兴趣.但对长江口外的上升流现象研究的还很少.目前只有少数简短的报道1)[1],也没有进行深入的研究和论证.与三峡工程有关的长江口海区的调查资料表明,在长江口外,水深为20～40m的区域内,也存在着较强的上升流现象.据此,笔者进一步查阅了长江口中美合作调查和全国海洋普查等资料.
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Le K entang.A Preliminary study of influence of ECSCC and TWC on CAW in summer in:Physics of Edited by Wang Huatong,Wang Jingyong,Dai Hua,China Ocean Press,(1990),231-241 Limeburner R,Beardsley R C and Zhao Jinsan,Water masses and circulation in the East China Sea.Proceedings of International Symposions on Sciimentation on the Continental Shelf with Special Reference to the East China Sea,Beijing,China,China Ocean Press,261-269 Hsueh Y and J J O'Brien.Steady coastal upwelling inducced by an along shore current,J,Phys.Oceangr 1971,1(3):180-186 Weaver A J and W W Hsieh,The Influence of buouancy flux from estuaries on continental shelf circulation,J.Phys.Oceangr.,1987,17(11):2127-2140 郭炳火,左海滨.海底漂浮物初步实验.黄渤海海洋,1984,2(2):71-74 蓝淑芳,傅秉照.南黄海和东海人工水母投放试验.海洋科学,1989,(3):21-26 -
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