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长江口水流运动特性分析
引用本文:于东生,田淳,严以新. 长江口水流运动特性分析[J]. 水运工程, 2004, 0(1): 49-53
作者姓名:于东生  田淳  严以新
作者单位:1. 河南海大学海岸及海洋工程研究所,江苏,南京,210098
2. 长江水利委员会长江口水文水资源勘测局,江苏,太仓,215431
基金项目:国家自然科学基金资助项目,编号:50079003
摘    要:根据长江口ADCP实测断面水流资料,对长江口断面运动随时间变化情况进行了分析,结果表明,涨落潮流分离,落潮主流偏向右岸(南岸),涨潮主流偏向左岸(北岸),流速存在着明显的差异,低平潮和高平潮前后,在断面上有三个方向环流的产生。

关 键 词:长江口  科氏力  环流  流速分布
文章编号:1002-4972(2004)01-0049-05
修稿时间:2003-07-01

An Analysis of Current Characteristics at the Yangtze River Estuary
YU Dong-sheng ,TIAN Chun ,Yan Yi-xin. An Analysis of Current Characteristics at the Yangtze River Estuary[J]. Port & Waterway Engineering, 2004, 0(1): 49-53
Authors:YU Dong-sheng   TIAN Chun   Yan Yi-xin
Affiliation:YU Dong-sheng 1,TIAN Chun 2,Yan Yi-xin 1
Abstract:An analysis of the situation of sectional current movement with the change of time at the Yangtze River Estuary is carried out based on the real-surveyed data of sectional current with ADCP.The result shows that the currents of flood tide and ebb tide are separated,main current of ebb tide leans to the right shore(south shore),main current of flood tide leans to the left shore(north shore),flow velocities are different obviously,and circumfluences at three directions occur along the sectional direction.
Keywords:the Yangtze River Estuary  ADCP  flow field  velocity distribution
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