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长江下游感潮河段大洪水和特大洪水的形成及趋势
引用本文:芮孝芳.长江下游感潮河段大洪水和特大洪水的形成及趋势[J].水科学进展,1996,7(3):221-225.
作者姓名:芮孝芳
作者单位:河海大学水资源水文系 南京 210098
摘    要:分析了长江下游感潮河段大洪水和特大洪水高水位形成的水文因素,揭示了年最高水位今后一段时期内可能的变化趋势。主要结论是:该河段大洪水和特大洪水高水位的形成原因十分复杂,本世纪以来每次大洪水和特大洪水高水位的形成几乎都有其主要原因;该河段大洪水特大洪水高水位出现的频次有增加趋势;自1975年以来,年最高水位的均值呈明显的升高趋势,其主要原因是人类活动对防洪产生的负面影响,海平面上升也有一定的影响。

关 键 词:长江下游    感潮河段    大洪水    特大洪水    变化趋势    人类活动    海平面
收稿时间:1995-05-10

Formation and Change Trend of Large Flood in the Lower Tidal Reach of the Yangtze River
Rui Xiaofang.Formation and Change Trend of Large Flood in the Lower Tidal Reach of the Yangtze River[J].Advances in Water Science,1996,7(3):221-225.
Authors:Rui Xiaofang
Affiliation:Hohai University, Nanjing 210098
Abstract:Hydrological factors of formation of large flood in the lower tidal reach of the Yangtze River are analyzed,and change trend of large flood is revealed.Obtained conclusions are:(1) Formation of large flood in the river reach is very complex; (2) Occurrence frequency of large flood in the river reach has been increasing since 1900; (3) The mean value of the peak stage has been rising since 1975; and (4) Above the charct eristics of occurrence of large flood in the river reach are primarily affected by human activity and rise of sea level.
Keywords:large flood  change trend  human activity  rise of sea level  tidal reach  lower reach of Yangtze River  
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