摘要
根据１９５９～１９８１年间观测的温度资料，分析了南黄海和东海春、冬两季 温度逆转类型的分布及其形成原因。分析得出了春、冬两季形成温度逆转类型的原 因，在春季主要有平流一对流、风和冷暖水的相互侵入，而在冬季主要是暖平流的作 用。
Based on the temperature data from 1959 to 1981 in the South Yellow Sea and the East China Sea in spring and winter, the distribution of the inverse types of temperature and its formative causes are analysed in this paper. The results show that inverse types of temperature can be separately Caused by the advectionconvection, the wind and the intrusion of warm or cold waters along surface in spring and the warm advection in winter.
出处
《海洋科学》
CAS
CSCD
北大核心
1995年第1期35-39,共5页
Marine Sciences
基金
国家自然科学基金!编号49176254
关键词
南黄海
东海
温度
逆转类型
成因
海温
The South Yellow Sea and East China Sea, Inverse types of temperture, Formative cause
