摘要
利用１９９２年５月在南黄海获得的ＣＴＤ资料对该海域春季温、盐结 构特征进行了分析，结果表明：（１）春季，南黄海温、盐结构处于由冬季型向 夏季型的过渡期，此时，整个研究海域大体上可以 ２０ｍ层为界分为上、下两 层。上表层的温、盐结构已基本呈现夏季型特征，但深底层还具有冬季型的 某些特征。（２）南黄海春季温、盐结构特征与水团配置具有较密切的关系，亦 即不同的温、盐结构对应着不同的水团，反之，同一个水团具有相近的温、盐 结构。
The characteristics of thermohaline structures in the South Yellow Sea in spring are analyzed based on CTD data observed in this sea area in May, 1992. The results are as follows: 1. In spring, the thermohaline structures in the South Yellow Sea are in a transitional period from the winter pattern to the summer pattern. At this time, the water in the whole area can be divided into upper layer and lower layer using approximately 20m depth as a demarcation. The structures of temperature and salinity in the upper surface layer show basically the characteristics of the summer pattern, but those in the lower.bottom layer are still of some properties of the winter pattern. 2. The characteristics of thermohaline structures are in close relationship with the distributions of water masses, that is, the different structures of temperature and salinity are corresponding with the different water masses, conversely, the,same water mass has the similar thermohaline structures.
出处
《海洋科学》
CAS
CSCD
北大核心
1994年第6期50-55,共6页
Marine Sciences
关键词
南黄海
盐结构
水团
温度
The South Yellow Sea, Thermohaline structures, Water masses
