摘要
利用中韩“黄海水循环动力学及物质输运”合作研究项目第一航次１９９６初春所获得的ＣＴＤ资料描述了南黄海初春温、盐和密度的水平和垂直分布特征，分析了水团结构，并揭示了春季在３４°～３６°Ｎ，１２１°４５’～１２４°Ｅ的南黄海西部水域的中层冷水现象．分析结果表明初春黄海暖流上表层开始向济州岛方向退缩，黄海底层冷水团首先在青岛外海形成．
ぉy using the CTD data obtained from the first cruise in the early spring of 1996 of 'China-Korea Ocean Circulation Dynamoics and Material Transportation Jpint Study on the Southern Huanghai Sea', the hoand vertical distributions of temperature, salinity and density are depicted, the analyses of water masses are made, and the formation mechanism of intermediate cold water (ICW) phenomenon which occUrred in the sea area west of the leathern Huangho Sea (34°-36°N, 121°45' -124°E) is revealed as well. The results also show that the Huanghai Sea Warn Current (YWW) in the surface regressed towards the Chejudo, and the Huanghai Sea Bottom Cold Water Mass (YC) began to form Only in the sea area off the Qingdao.
出处
《海洋学报》
CAS
CSCD
北大核心
2000年第1期17-26,共10页
基金
国家海洋局和国家自然科学基金!49676283
关键词
水文特征
中层冷水
水团特征
黄海暖流
Hydrographic features, intermediate cold water, the characteristics of water mass, the Huanghai Sea Warm Current
