摘要
本文分别对位于台湾海峡中部和北部两个连续观测站１９９８年２～３月的ＣＴＤ资料进行分析，认为北部测站在观测期间经历了低温、低盐水入侵的过程，但此过程只显著影响到３０ｍ层，温盐垂直结构有时出现单跃层，有时出现阶梯结构；而中部测站盐度垂直均匀，温度垂直梯度也较小，已不受闽浙沿岸水的影响。
Through an analysis on the CTD data from two time series anchored stations in the central and northern Taiwan Strait during February - March 1998, it is concluded that: the vertical structure of temperature and salinity at the northern station and the central station can be classified into 2 types, respectively; the northern station undergoes an invasion process of low temperature and low salinity water during the period of investigation, but the remarkable effect can only be seen at 0-30m depth; and the central station can not be affected by the Minzhe Coastal Water.
出处
《海洋湖沼通报》
CSCD
北大核心
1999年第4期8-13,共6页
Transactions of Oceanology and Limnology
基金
国家自然科学基金重点项目资助!49636220
关键词
台湾海峡
温度
盐度
日变化过程
Central and northern Taiwan Strait, temperature, salinity
