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长江口浑浊带核心区北槽水动力特征研究

蒋杰 何青 朱磊 林建良

蒋杰, 何青, 朱磊, 林建良. 长江口浑浊带核心区北槽水动力特征研究[J]. 海洋学报, 2019, 41(1): 11-20. doi: 10.3969/j.issn.0253-4193.2019.01.002
引用本文: 蒋杰, 何青, 朱磊, 林建良. 长江口浑浊带核心区北槽水动力特征研究[J]. 海洋学报, 2019, 41(1): 11-20. doi: 10.3969/j.issn.0253-4193.2019.01.002
Jiang Jie, He Qing, Zhu Lei, Lin Jianliang. Analysis of hydrodynamic features of the North Passage in the turbidity maximum, Changjiang Estuary[J]. Haiyang Xuebao, 2019, 41(1): 11-20. doi: 10.3969/j.issn.0253-4193.2019.01.002
Citation: Jiang Jie, He Qing, Zhu Lei, Lin Jianliang. Analysis of hydrodynamic features of the North Passage in the turbidity maximum, Changjiang Estuary[J]. Haiyang Xuebao, 2019, 41(1): 11-20. doi: 10.3969/j.issn.0253-4193.2019.01.002

长江口浑浊带核心区北槽水动力特征研究

doi: 10.3969/j.issn.0253-4193.2019.01.002
基金项目: 国家自然科学基金项目(51320105005,51739005);国家重点研发计划(2016YFE0133700);上海市科委重点项目(17DZ1204801)。

Analysis of hydrodynamic features of the North Passage in the turbidity maximum, Changjiang Estuary

  • 摘要: 本文根据2015年长江口洪季浑浊带水域座底三脚架全水深范围观测数据,对北槽中下段纵横向流、余流结构、边界层特征等进行了深入研究,结果显示:(1)大潮潮流矢量特征在垂向上的变化差异最为显著;北槽中下段水流出现明显的横向输移,指向航槽北面;(2)横向流速在大潮期间的变化(垂线平均)为-0.10~0.39 m/s,小潮期间的变化为-0.13~0.25 m/s;横向平流对于北槽纵向物质输运有显著调整作用;(3)余流垂向差异大,底部几乎为0,小潮期间余流更强;周期性再悬浮的细颗粒泥沙可作为北槽最大浑浊带的重要物质来源;(4)传统六点对数流速拟合法获得摩阻流速误差较大,近底1 m区域高分辨流速剖面是准确获取底边界层参数的有效途径。
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出版历程
  • 收稿日期:  2017-12-06
  • 修回日期:  2018-04-27

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