论文部分内容阅读
台湾海峡是东海和南海间的水通道,过去从季风场的观点出发,认为海峡区的表层流属于季风性质的风漂流。近年来研究表明,上述结论已不符合实际情况,而是海峡区的海水运动和水文特征,直接受黑潮支流、南海水和近岸水系强弱的影响,因而水文特征较为复杂,如果采用水文要素的多年平均值,则不易看出其明显特征。本文采用1960年以后的CSK以及有关的海洋调查资料,根据温盐和条件密度的空间分布、等σ_t面的流型分析对本海区的流
The Taiwan Strait is a water passage between the East China Sea and the South China Sea. In the past, from the viewpoint of the monsoon field, it is considered that the surface currents in the Strait are of the monsoon type. In recent years, studies have shown that these conclusions are not in line with the actual situation, but the sea area of the Straits sea movement and hydrological characteristics, directly affected by the Kuroshio tributaries, the South China Sea and coastal water system strength and weakness, hydrological characteristics are more complex, if the use of hydrology Elements of the multi-year average, it is not easy to see its obvious characteristics. In this paper, the CSK after 1960 and the relevant marine survey data are used to analyze the flow in the sea area based on the spatial distribution of temperature, salt and conditional density,