Hydroclimate Analysis of Severe Floods in China's Poyang Lake Region

被引:30
作者
Shankman, David [1 ]
Keim, Barry D. [2 ]
Nakayama, Tadanobu [3 ]
Li, Rongfang [4 ]
Wu, Dunyin [5 ]
Remington, W. Craig [6 ]
机构
[1] Univ Alabama, Dept Geog, Tuscaloosa, AL 35487 USA
[2] Louisiana State Univ, Dept Geog & Anthropol, Baton Rouge, LA 70803 USA
[3] Ctr Global Environm Res, Tsukuba, Ibaraki, Japan
[4] Jiangxi Inst Water Sci, Nanchang, Peoples R China
[5] Jiangxi Normal Univ, Nanchang, Peoples R China
[6] Univ Alabama, Cartog Res Lab, Tuscaloosa, AL 35487 USA
关键词
ENSO; Floods; China; Poyang Lake; Yangtze River; YANGTZE-RIVER BASIN; TRENDS;
D O I
10.1175/2012EI000455.1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Poyang Lake in Jiangxi Province is the largest freshwater lake in China and is historically a region of significant floods. Maximum annual lake stage and the number of severe flood events have increased during the past few decades because of levee construction that reduced the area available for floodwater storage. The most severe floods since 1950 occurred during 1954, 1973, 1983, 1995, and 1998. Each of these floods followed El Nino events that influence the Asian monsoon and that are directly linked to rainfall in the Changjiang (Yangtze River) basin. The 1954 flood was the largest ever recorded until the 1990s. That year the peak Changjiang stage at Hukou was 21.6 m, which was 1.6 m above the previous record high. The last major flood on the Changjiang was during 1998, when the peak Changjiang stage reached 22.5 m, higher than during 1954, even though peak discharge was lower. The most severe floods, including those in 1954 and 1998, require both 1) high rainfall and tributary discharge into Poyang Lake and 2) high Changjiang discharge and stage at Hukou that backflows into the lake or slows Poyang Lake drainage. Since gauging stations were established on the Changjiang, these conditions always occurred following an El Nino.
引用
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页码:1 / 16
页数:16
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