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

AbstractPoyang 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 P...

[1]  J. Milliman,et al.  Seasonal variations of sediment discharge from the Yangtze River before and after impoundment of the Three Gorges Dam , 2009 .

[2]  Zhongyuan Chen,et al.  Anastomosing river system along the subsiding middle Yangtze River basin, southern China , 2005 .

[3]  Guofeng Wu,et al.  Concurrent monitoring of vessels and water turbidity enhances the strength of evidence in remotely sensed dredging impact assessment. , 2007, Water research.

[4]  R. Edmonds The Sanxiadz (Three Gorges) Project : the environmental argument surrounding China's super dam , 1992 .

[5]  Kevin E. Trenberth,et al.  The Definition of El Niño. , 1997 .

[6]  Tong Jiang,et al.  Recent trends in observed temperature and precipitation extremes in the Yangtze River basin, China , 2006 .

[7]  Y. Zong,et al.  The 1998 Flood on the Yangtze, China , 2000 .

[8]  Chen Chuan,et al.  An analysis of the variation of maximum flood stage of Lower Yangtze River , 2003 .

[9]  Poojitha D. Yapa,et al.  A model for simulating deep water oil and gas blowouts - Part II: Comparison of numerical simulations with “Deepspill” field experiments , 2003 .

[10]  J. de Leeuw,et al.  River management, landuse change, and future flood risk in China's Poyang Lake region , 2009 .

[11]  T. Nakayama,et al.  Role of flood storage ability of lakes in the Changjiang River catchment , 2008 .

[12]  Chengming Wen,et al.  Recent advances in studies of the interaction between the East Asian winter and summer monsoons and ENSO cycle , 2004 .

[13]  Shaowu Wang,et al.  A Comparison between Observed and GCM-Simulated Summer Monsoon Characteristics over China , 1995 .

[14]  Y. Jie,et al.  YANGTZE DYKE AND ITS STRENGTHENING , 2003 .

[15]  Xin‐Zhong Liang,et al.  Understanding relationships between the 1998 Yangtze River flood and northeast Eurasian blocking , 2003 .

[16]  Tong Jiang,et al.  Interactions of the Yangtze river flow and hydrologic processes of the Poyang Lake, China , 2007 .

[17]  Zhaoyin Wang,et al.  Sediment budget of the Yangtze River , 2007 .

[18]  Erich J. Plate,et al.  Recent flood disasters in China , 2002 .

[19]  James W. Burnham,et al.  Strategic assessment of the magnitude and impacts of sand mining in Poyang Lake, China , 2010 .

[20]  Jie Song,et al.  Flood frequency in China's Poyang Lake region: trends and teleconnections , 2006 .

[21]  Xia Jun,et al.  Water problems and opportunities in the hydrological sciences in China , 2001 .