一、前言 台风强风对海洋开发、海上交通、渔业及海上军事活动等有着极大的影响.近年来已经有不少人研究台风风场数学模式,但这些模式大多仅适用于轴对称风场分布的静止台风.美国目前广泛采用Wilson提出的移行风暴梯度风方程求飓风风场,而日本等国则普遍运用宫崎正卫等人求台风合成风的假设.这二种计算海面风的方法都比较冗繁, I. INTRODUCTION Strong winds of typhoon have great influence on marine development, maritime traffic, fishery and maritime military activities, etc. Many people have studied mathematical models of typhoon wind fields in recent years, but most of these models are only applicable to the distribution of axisymmetric wind fields The stationary typhoon in the United States is widely used by the United States nowadays.However, Japan and other countries generally use the assumption that typhoon Yoshinori Miyazaki and others are seeking typhoon winds.Two methods for calculating sea surface wind More complicated,