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象山港潮波响应和变形研究 Ⅲ.潮滩位置和平流效应对M4分潮的作用
引用本文:董礼先,苏纪兰,王丽娅.象山港潮波响应和变形研究 Ⅲ.潮滩位置和平流效应对M4分潮的作用[J].海洋学报,1999,21(3):1-6.
作者姓名:董礼先  苏纪兰  王丽娅
作者单位:1.国家海洋局第二海洋研究所, 杭州 310012
基金项目:国家自然科学基金!48907026
摘    要:通过半封闭矩形理想海湾的潮波运动数值模拟,分析了潮滩及平流效应对M4分潮的生成和增长的影响.结果说明潮滩的作用不但依赖本身的规模和湾内潮波非线性的强弱,而且与潮滩在湾内所处位置关系很大.在存在M4分潮共振的海湾中,平流效应可以抑制共振对M4分潮的放大作用.

关 键 词:M4分潮    数值模型    共振    平流
收稿时间:1997/11/8 0:00:00
修稿时间:1998/6/18 0:00:00

Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay
Dong Lixian,Su Jilanic and Wong Li Ah.Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay[J].Acta Oceanologica Sinica (in Chinese),1999,21(3):1-6.
Authors:Dong Lixian  Su Jilanic and Wong Li Ah
Institution:1.Second institute of Ocmnography, State Oceanic Administration, Hangzhou 3100122.Hong Kong Un University fo Science and Technology, Kowloon, Hong Kong
Abstract:The contribution of the tidal flat and tidal currents advection to the generation and growth of M4 tidal component isanalyzed by using a numerical modelling in a ideal semi-enclosed rectanglular bay. The result shows that the contribution of tidal flatdepends not only on the location and dimension of the tidal flat, but also on the non-linearity of the tide in the bay. The amplitudeof the M4 tidal component is inhibited by the advection in the bay where there is the M4 tide co-oscillation.
Keywords:M4 tide  numerical modelling  co-oscillation  advection
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