摘要
用１９８３年１１月在黄、东海调查的水文观测资料，分析了该海区温、盐度 垂直分布类型的地理分布，详细地讨论了秋季温、盐度逆转现象的形成原因。分析 得出，在研究海区内，引起温、盐度逆转现象的原因有：（１）海面失热冷却产生的垂 直对流作用；（２）秋季季风已转变为北风，在北风（特别是北风大风）的驱动下，迫使 表层水向南向外扩张的影响；（３）深层暖平流（台湾暖流和黄海暖流）向岸向北伸展 或切入的影响；（４）在锋区，高温（或低温）高盐（或低盐）水沿等面扩展的影响。
In this paper, using data observed in November 1983, geographical distributions of vertical structure types of temperature and salinity in the Yellow Sea and East China Sea are described, and the causes of inverse phenomena of temperature and salinity are discussed in great detail. The results show that the causes of inverse phenomena are: (1) the effect of vertical convection which is caused by cooling sea surface water, (2) the effect of expend and variation of surface water which are forced by northerly wind, (3) the effect of warm advection (Taiwan Warm Current and Huanghai Warm Current), and (4) the effect of intrusion of warm or cold water along . surface.
出处
《海洋科学》
CAS
CSCD
北大核心
1994年第2期47-51,共5页
Marine Sciences
基金
国家自然科学基金资助项目!编号49176254
关键词
东海
秋季
温度
盐度
分布
黄海
The yellow sea and East china sea, Autumn, Temperature and salinity,Inverse Phenomena
