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长江河口涨落潮不对称性动力成因分析
A study on the dynamics of the asymmetry between flood and ebb in the Changjiang Estuary
【摘要】 长江河口存在着涨落潮流速和历时的不对称现象。本应用长江河口三维数值模式,数值试验定量给出了不同径流量、潮汐和水深下南北支、南北港和南北槽涨潮落潮平均流速和历时,通过横断面涨潮落潮通量必须满足质量守恒观点从动力机制上给出了涨潮落潮流速和历时不对称的成因。
【Abstract】 There exists the asymmetry of current speed and duration between flood and ebb in the Changjiang Estuary.Applied the three-dimension numerical model in the Changjiang Estuary,the mean flood/ebb current speed and duration in the South/North Branch,South/North Channel and South/North Passage under different river discharges,tide and water depth were given out quantitatively by the numerical experiments.The dynamic causes of the asymmetry of flood/ebb current speed and duration are explained in the view of mass conservation by the water flux through the transect during flood and ebb period.
【Key words】 Changjiang Estuary; flood-ebb asymmetry; river discharge; tide; numerical experiments;
- 【文献出处】 海洋学报(中文版) ,Acta Oceanologica Sinica , 编辑部邮箱 ,2011年03期
- 【分类号】P343.5
- 【被引频次】23
- 【下载频次】535