摘要
以 1 975～ 1 999年夏季东海标准断面观测资料为据 ,把东海 30°N断面的盐度分布态势划分成 4个类型 ,并以 1 975～ 1 985年的大面资料为主 ,初步讨论了对应于这 4个类型的长江冲淡水扩散形态与台湾暖流水的强弱、位置等的关系。结果表明 :多数分布类型都具有代表性的冲淡水分布态势 ;长江冲淡水的扩散形态似与台湾暖流的北伸强弱、离岸远近、离表面的深浅有较密切的关系。
Based on the summer's standard sectional data at the 30°N profile in 1975-1999,the salinity distribution has been divided into four types.The four salinity distribution types on the relation of the spreading forms of the Changjiang River diluted water with Taiwan warm water's strength and its position were primarily discussed on the basis of mainly the salinity data of 1975-1985.It is found that most of the salinity types exist in the representative features of diluted water seem to be closely connected with the Taiwan warm current's northward spreading strength,its distance from the coast and its depth to the sea surface.
出处
《东海海洋》
2002年第1期1-13,共13页
Donghai Marine Science
关键词
东海
盐度
长江冲淡水
台湾暖流水
夏季
扩散形态
East China Sea
salinity
spreading
Changjiang River dilued water
Taiwan warm current's water
