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极浅海域潮流数值模型
引用本文:张存智,杨连武,窦振兴. 极浅海域潮流数值模型[J]. 海洋与湖沼, 1994, 25(6): 671-676
作者姓名:张存智  杨连武  窦振兴
作者单位:国家海洋局海洋环境保护研究所!大连,116023,国家海洋局海洋环境保护研究所!大连,116023,国家海洋局海洋环境保护研究所!大连,116023
摘    要:通过对以往的浅水环流数值模型进行改进,建立适用于极浅水域的且能达到较高分辨率的潮汐环流数值模型。模型的主要特点是:(1)通过改进海底摩擦项的表达式来克服传统的二次方律在极浅的潮滩区所产生的不稳定问题;(2)采用逆风格式处理动量方程中的平流项,有效地抑制由于岸边界移动引起的数值短波的扩散。结合老虎滩湾海上工程的需要,利用本模型进行一系列的数值模拟试验。经过实测资料验证表明,改进后的模型具有良好的稳定

关 键 词:极浅海域 潮流 数值模型
收稿时间:1992-07-11
修稿时间:1993-02-20

A NUMERICAL MODEL OF TIDAL CURRENT IN EXTRA-SHALLOW WATERS
Zhang Cunzhi,Yang Lianwu and Dou Zhenxing. A NUMERICAL MODEL OF TIDAL CURRENT IN EXTRA-SHALLOW WATERS[J]. Oceanologia Et Limnologia Sinica, 1994, 25(6): 671-676
Authors:Zhang Cunzhi  Yang Lianwu  Dou Zhenxing
Affiliation:Institute of Marine Enrironmental Proiection, SOA, Daliah 116023;Institute of Marine Enrironmental Proiection, SOA, Daliah 116023;Institute of Marine Enrironmental Proiection, SOA, Daliah 116023
Abstract:A high resolution tidal current numerical model suitable for extrashallow wate-rs was developed by improving the previous numerical model of shallow water ci-rculation. The main points of the improved model are: (1) The expression of the bottom friction terms in the momentum equations are modified in order to overco-me the instability resulting from the application of the traditional square law in the extra-shallow tidal flat area. (2) The up-wind scheme is used to deal with the ad-vection terms in the momentum equations, so that the dispersion of the numerical short waves due to the moving of the land-water boundaries is restrained effective-ly. A finite difference method is used to solve the model equation. The computatio-nal grid is staggered. The timestepping procedure is based on the implicit alternate direction approach. The thomas algorithm is used to solve the tridiagonal system.Agreement between the model results and the observed data in numerical modelling experiments carried out in Laohutan Bight indicated that the improved model has good stability and reproducibility.
Keywords:Extra-shallow waters Tidal current Numerical model  
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