摘要
通过南海北部湾北部海域的温、盐及重力势资料分析,地转流场表明,该海域在春季存在一个反时针的密度环流.认为该环流的形成机制,主要是热力作用的结果,各海域受热升温速度不一,而残存着冬季的冷水所致.环流强度较弱.存在时间短,春生夏消.
Based on temperature, salinity and geopotential height data of the northern Beibu Gulf of the South China Sea. the analysis of the geostrophic current shows there is a cyclone circulation in northern Beibu Gulf in Spring. It is considered that the Circulation is formed by heating power, the different temperature in different areas and the survival cold water after winter in the deep sea. The circulation is feeble and has short duration, occurring in spring and disappearing in summer.
出处
《海洋通报》
CAS
CSCD
北大核心
1995年第1期81-85,共5页
Marine Science Bulletin
关键词
海湾
气旋式环流
热力学
环流
cyclone circulation
thermodynamics
Beibu Gulf
