一、引言关于黄海潮波的数值模拟,我国、苏联、南朝鲜等学者都有不少的研究.模拟的方法,一般采取边值法和直接求解潮波原始方程组,即H-N方法两种.我国已有作者在渤海用H-N方法进行了计算.南朝鲜的崔秉昊用这种方法做了整个东中国海主要日潮和半日分潮的数值模拟,并进行了比较详细的描述,但他的计算在朝鲜沿岸比较准确,在中国沿岸误差较大.为了通过计算更深刻地认识黄、渤海区的潮汐潮流特征,特别是中国一侧的特征,并给某些小范围的数值模拟提供水界边界条件,我们进行 I. INTRODUCTION There are quite a few researches on the numerical simulation of the Yellow Sea tide waves in China, the Soviet Union and South Korea, etc. The simulation methods generally adopt the boundary value method and the direct solution of the tidal wave original equations, that is, two kinds of HN methods. Our country has been calculated by the HN method in the Bohai Sea, and Cui Bing-hao, from South Korea, used this method to do numerical simulations of the major tidal and semi-diurnal tides over the entire East China Sea. However, his calculations It is more accurate on North Korea coast and larger on the coast of China. In order to understand the characteristics of tide tidal current in the Yellow Sea and Bohai Sea area, especially on the Chinese side, and to provide some small-scale numerical simulation with boundary conditions of water boundary We do it