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南黄海和东海春、冬季温度逆转类型的分布及其成因分析
引用本文:丁宗信,蓝淑芳.南黄海和东海春、冬季温度逆转类型的分布及其成因分析[J].海洋科学,1995,19(1):35-39.
作者姓名:丁宗信  蓝淑芳
作者单位:中国科学院海洋研究所!青岛266071
基金项目:国家自然科学基金!编号49176254
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。分析得出春、冬两季形成温度逆转类型的原因,在春季主要有平流-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。

关 键 词:南黄海  东海  温度  逆转类型  成因  海温
收稿时间:1994/3/20 0:00:00

A PRELIMINARY ANALYSIS OF THE DISTRIBUTION OF THE INVERSE TYPES OF TEMPERATURE AND ITS FORMATIVE CAUSES IN THE SOUTHERN YELLOW SEA AND THE EAST CHINA SEAS IN SPRING AND WINTER
Ding Zongxin and Lan Shufang.A PRELIMINARY ANALYSIS OF THE DISTRIBUTION OF THE INVERSE TYPES OF TEMPERATURE AND ITS FORMATIVE CAUSES IN THE SOUTHERN YELLOW SEA AND THE EAST CHINA SEAS IN SPRING AND WINTER[J].Marine Sciences,1995,19(1):35-39.
Authors:Ding Zongxin and Lan Shufang
Abstract: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.
Keywords:The South Yellow Sea and East China Sea  Inverse types of temperture  Formative cause
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