摘要
本文着重分析了1987年和1988年5～8月的温、盐度观测资料,并与1983年6～8月和1984年5月的观测资料进行对比,结果表明,台湾海峡中、北部海域春、夏季(5～8月)温、盐度结构主要取决于不同季风的影响。季风的转换过程既是海域温、盐结构调整过程,也是海域上升流形成过程。
Temperature and salinity data surveyed from May to August of 1987 and 1988 are ana-ysed and compared with the data from June to August of 1983 and May of 1984. The result shows that monsoon affects the temperature and salinity structure in spring and summer (May to August) in North Central Taiwan Strait. In this area process of monsoonal change is the process of regulating temperature and salinity structure and is also the process of forming upwelling.
出处
《海洋科学》
CAS
CSCD
北大核心
1991年第4期53-57,共5页
Marine Sciences
关键词
台湾海峡
温度
盐度
上升流
季风
Monsoon, Structure of temperature and salinity, Upwelling
