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长江口斜压诊断模式三维流场数值模拟
引用本文:龚政,张长宽,金勇,张东生.长江口斜压诊断模式三维流场数值模拟[J].水科学进展,2004,15(3):300-306.
作者姓名:龚政  张长宽  金勇  张东生
作者单位:1.水利部太湖流域管理局水利发展研究中心, 上海, 200434;
基金项目:水利部科技创新项目(CSX2000 57),教育部科技研究重点项目(01100)
摘    要:建立了σ坐标系下长江口斜压诊断模式三维流场数学模型,采用k-kl二方程紊流闭合模型求解垂向涡粘系数,计算域内恒定、非均匀盐度场反映了计算域密度斜压效应。验证结果表明,斜压诊断模式的模拟成果较切合实际。模型成功复演了长江口水域由往复流向旋转流过渡的流场特性;潮波从四条汊道传入后在分汊口附近相遇形成多个会潮点,其位置随着径流的大小、潮汐的强弱、汊道的形态等因素而变化。

关 键 词:长江口    斜压诊断模式    三维流场    数值模拟
文章编号:1001-6791(2004)03-0300-08
收稿时间:2003-03-06
修稿时间:2003年3月6日

3-D current numerical model for the Yangtze River estuary with baroclinic-diagnosis mode
GONG Zheng,ZHANG Chang-kuan,JIN Yong,ZHANG Dong-sheng.3-D current numerical model for the Yangtze River estuary with baroclinic-diagnosis mode[J].Advances in Water Science,2004,15(3):300-306.
Authors:GONG Zheng  ZHANG Chang-kuan  JIN Yong  ZHANG Dong-sheng
Affiliation:1.Water Resources Development Research Center, Taihu Basin Authority, Shanghai 200434, China;2.College of Traffic and Ocean Engineering, Hohai University, Nanjing 210098, China;3.Shanghai Designing Institute of Reconnaissance, Shanghai 200434, China
Abstract:This paper presents a 3-D current numerical model for the Yangtze River estuary with baroclinic-diagnosis mode in vertical σcoordinate system.A vertical eddy-viscosity coefficient is obtained from the advanced k-kl turbulence closure model, and the density baroclinic effects are embodied by the 2-D invariable-uneven salinity field.It shows the results from baroclinic-diagnosis mode well consistent with reality.The transition feature from back and forth current to rotary current is re-acted successfully.In addition,several tidal junction points appeare near branch points when tidal wave propagate from four river forks, the position of which change with runoff,tide and topography.
Keywords:Yangtze River estuary  baroclinic-diagnosis mode  3-D current  numerical model
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