论文部分内容阅读
本文主要根据韩国海洋研究所通过东海沿岸海洋过程试验（即COPEX－ECS）收集的CTD资料，较详细地研究了东海东北部夏季的水文状况．文中首先分析了夏季出现在该海域最重要的几件海洋现象．其中主要包括长江冲淡水的东向扩展，黄海底层冷水南向插入，以及黑潮水的爬升和渗透。然后，使用t－S分析法，并参考有关研究成果，对东海东北部夏季水团进行了划分，并重点探讨了黑潮水和对马暖流水的结构特征。最后，本文讨论了朝鲜／对马海峡东、西水道夏季水文结构的差异问题。
In this paper, we mainly studied the hydrological conditions in the northeast of the East China Sea in more detail based on the CTD data collected by the Korea Ocean Research Institute through the East China Sea Coastal Ocean Experiment (COPEX-ECS). The article first analyzes the most important marine phenomena that appear in the sea in summer. These include the eastward expansion of the red water in the Yangtze River, the insertion of cold water at the bottom of the Yellow Sea, and the climb and infiltration of Kuroshio water. Then, by using t-S method and referring to relevant research results, the summer water mass in the northeast of East China Sea was divided, and the structural characteristics of Kuroshio and Mamanguchi were discussed. Finally, the paper discusses the differences in the summer hydrological structure between North Korea and the East and West Sewers of the Strait of the Strait.