摘要
采用1987年5-6月中日合作黄东海海域综合调查溶解氧资料,参考有关文献,讨论调查海域溶解氧分布特征及与水团的对应关系。分析结果表明,各水团中溶解氧含量的差异与各水团温盐特性及生物地球化学过程不同有关。通过分析还发现溶解氧对鉴别次表层以深各水团,特别对东海次表层水及黑潮次表层以深各水团,是一个重要的指标。
Analysis of dissolved oxygen data obtained the China-Japan Joint Survey in the Yellow Sea and East China Sea from May to June 1987, and other data to derive the relatinship between the dissoved oxygen distribution and water masses there showed that the dissolved oxygen content differences in different water masses is due to the differences of temperature, salinity, and biogeochemical processes in different water masses. The dissolved oxygen distribution is an indicator of , and controled by, water object movement, is a usable index to differentiate water masses that lie in under the subsurface water masses, especially those that lie in under the East China Sea Subsurface Water Mass and the Kuroshion Subsurface Water Mass.
出处
《海洋与湖沼》
CAS
CSCD
北大核心
1995年第S1期47-53,共7页
Oceanologia Et Limnologia Sinica
基金
国家教委中日合作东中国海水团分布机制多学科调查研究课题!4701
关键词
溶解氧分布
水团
春末
黄东海海域
Distribution dissolved oxygen Water mass Late spring Sea area of Yellow Sea and East China Sea