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黑潮是北太平洋西部的强大暖流。它将海洋在低纬海区接收到的大量太阳辐射热,带向中高纬海区,并通过潜热和感热的形式,将热量传给大气。由于黑潮流域宽广,从低纬向中高纬输送热量的多少,不仅会对东海及邻近大洋的水文要素产生较大的影响,而且还会引起巨大的海——气之间热量收支的变异,从而可能使大气环流发生相应的变化。因此,对黑潮的研究,不仅海洋学者十分重视,气象学者也对此产生了浓厚的兴趣。如wrytki(1965)、Hastenrath(1977)等人曾对太平洋海洋与大气的热量平衡进行过计算和分析,KOPT(1970)计算了黑潮热含量,讨论了它与西风环流指数的关系。我国大气所、地理所等单位也
Kuroshio is a powerful warm current in the western North Pacific. It takes a large amount of solar radiation heat that the ocean receives in the low latitude sea area to the mid-high latitude sea area and transmits the heat to the atmosphere through latent heat and sensible heat. Owing to the broad Kuroshio watershed, the amount of heat transferred from the low latitudes to the middle and high latitudes will not only have a great impact on the hydrological elements in the East China Sea and the adjacent oceans, but will also cause huge sea-and-gas heat budget variations , Which may make the atmospheric circulation corresponding changes. Therefore, not only oceanographers have paid much attention to the study of Kuroshio, but meteorologists also have a keen interest in it. For example, Wrytki (1965) and Hastenrath (1977) have calculated and analyzed the thermal balance between ocean and atmosphere in the Pacific Ocean. KOPT (1970) calculated the Kuroshio heat content and discussed its relationship with the westerly circulation index. China’s atmosphere, geography and other units also