摘要
1994 年11 月 24—25 日 (枯季), 在长江口南部水域内, 对 2 个定点、2 个段面 ( 24 个站位) 进行了水流流速、盐度及悬沙浓度观测。而后,分别绘制出:( 1 ) 水流流速、盐度和悬沙浓度沿水深、时间变化过程图;( 2 ) 各层水流流速、流向随时间变化过程图。 结果分析表明: 1 ) 实测水流流速、盐度及悬沙浓度垂向、水平分布具不连续性,表明了次级羽状锋的存在; 2 ) 在枯季,相对于径流、波浪而言, 外海潮流对长江口次级羽状锋的影响占主导作用; 3 ) 次级羽状锋可能使得悬沙在南汇东滩附近大量淤积;4)次级羽状锋在长江口与杭洲湾之间的水沙交换中起着一定作用。
:Tidal current velocity, salinity and suspended sediment concentration have been measured at two monitoring stations and along two transects (1994-11-24~-25) in the southern waters of the Changjiang River estuary. Two types of plots have been obtained: (1) time series of current velocity, salinity and suspended sediment concentration (contour lines); (2) time series of current speed and direction measured at six different depths. Those data suggest that 1) the secondary Changjiang River plume is present; 2) the tidal current appears to be a dominant mechanism for the secondary Changjiang River plume during dry season; 3) the secondary Changjiang River plume could result in the deposition of fine suspended sediments on the Nanhui tidal flat; and 4) the secondary Changjiang River plume also plays an important role in the water and sediment exchange between the Changjiang River estuary and the Hangzhou Bay.
出处
《海洋通报》
CAS
CSCD
北大核心
2002年第6期1-8,共8页
Marine Science Bulletin
基金
国家自然科学基金 (49806005)
国家教育部跨世纪优秀人才培养计划基金资助
关键词
长江口
次级羽状锋
水流流速
盐度
悬沙浓度
杭州湾
:secondary plume
velocity
salinity
suspended sediment concentration
Changjiang River estuary