一、前言早在五十年代初,表面风应力的空间变化,已被作为基本量,讨论风生大洋环流。近来,海面风应力对海洋动力要素(海流、海浪、风暴潮等)的影响,更进一步引起了海洋学家们的重视,研究和计算风应力的文章也日益增多。 M·Peter(1976)利用1941—1972年累积的一百万次船舶报告资料,计算了北美东大陆 I. Introduction As early as the early 1950s, the spatial variation of surface wind stress has been used as a basic volume to discuss the wind and ocean currents. Recently, the influence of sea surface wind stress on ocean dynamic elements (currents, waves, storm surges, etc.) further aroused the attention of oceanographers and articles on the study and calculation of wind stress are also increasing. M Peter (1976) used the accumulated shipments of millions of ships from 1941 to 1972 to calculate the North East Asian continent