Spatiotemporal variations of inter- and intra-annual extreme streamflow in the Yangtze River Basin

被引:5
|
作者
Huang, Anqi [1 ,2 ]
Gao, Guangyao [1 ,2 ]
Yao, Liqiang [3 ]
Yin, Shihua [1 ,2 ]
Li, Dongfeng [4 ]
Do, Hong Xuan [5 ]
Fu, Bojie [1 ,2 ]
机构
[1] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Yangtze River Sci Res Inst, Water Resources Dept, Wuhan 430010, Peoples R China
[4] Peking Univ, Coll Environm Sci & Engn, Key Lab Water & Sediment Sci, Minist Educ, Beijing 100871, Peoples R China
[5] Nong Lam Univ Ho Chi Minh City, Fac Environm & Nat Resources, Ho Chi Minh City, Vietnam
基金
中国国家自然科学基金;
关键词
Extreme streamflow; Muti-temporal scales; Climate change; Dams; Large river basin; SEDIMENT LOAD; OBSERVED TRENDS; WATER DISCHARGE; CLIMATE-CHANGE; ENSO; PRECIPITATION; FREQUENCY; FLOW; VARIABILITY; IMPACTS;
D O I
10.1016/j.jhydrol.2024.130634
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Climate change has led to anomalous fluctuations in extreme streamflow from global river systems, and the superposition of human activities such as damming has compounded the changes in extreme streamflow, affecting floods and river ecosystems. However, muti-temporal scale variations of extreme streamflow and the dominant driving factors were limitedly understood. In this study, we examined the changing patterns of interand intra-annual extreme (maximum 1 -day, consecutive 3 -days and 7 -days) streamflow (including magnitude and timing) in the Yangtze River Basin (YRB) from the 1940 s to 2020. Furthermore, the roles of ENSO events and dams on temporal anomalies of extreme streamflow at interand intra-annual scales were identified in the whole basin. We found that the annual streamflow extremes increased in the source YRB and the middle and lower YRB but decreased in the upper YRB. The extreme streamflow during spring and autumn was characterized by increasing trends in the source and decreasing trends in other reaches. The occurrence timing of winter extreme streamflow in the upper and middle YRB was significantly delayed. The inter -annual extreme streamflow in the source and upper YRB had a negative relationship with ENSO, while the positive relationship held in the middle and lower YRB. The major anomalies (>50 %) of annual extreme streamflow generally occurred in ENSO (1+2) yrs, while precipitation contributes to the seasonal distribution of extreme streamflow. There was a good correlation between precipitation and both annual and summer extreme streamflow in the lower YRB, but the relationship completely shifted in the upper YRB after 2003. Further, the construction of dams has severely affected extreme streamflow, leading to a stepwise drop in annual and summer/autumn flows and a sudden rise in spring/winter flows. This study facilitates the prediction of extreme streamflow and the development of sustainable basin management strategies.
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收藏
页数:15
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