Climate change drives flooding risk increases in the Yellow River Basin

被引:38
作者
Lan, Hengxing [1 ,2 ]
Zhao, Zheng [1 ,3 ]
Li, Langping [1 ,3 ]
Li, Junhua [4 ]
Fu, Bojie [5 ,6 ]
Tian, Naiman [1 ,3 ]
Lai, Ruixun [4 ]
Zhou, Sha [6 ]
Zhu, Yanbo [2 ]
Zhang, Fanyu [7 ]
Peng, Jianbing [2 ]
Clague, John J. [8 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing 100101, Peoples R China
[2] Changan Univ, Sch Geol Engn & Geomat, Xian 710064, Peoples R China
[3] Univ Chinese Acad Sci, Beijing, Peoples R China
[4] Yellow River Conservancy Commiss, Yellow River Inst Hydraul Res, Zhengzhou 450003, Peoples R China
[5] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Beijing, Peoples R China
[6] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resources Ecol, Beijing 100875, Peoples R China
[7] Lanzhou Univ, Sch Civil Engn & Mech, Key Lab Mech Disaster & Environm Western China, Minist Educ China, Lanzhou 730000, Peoples R China
[8] Simon Fraser Univ, Dept Earth Sci, Burnaby, BC, Canada
关键词
Flooding risk; Risk management; Climate change; Flood discharge; Extreme precipitation; SHIFTS; RAINFALL; EXTREME; STORMS;
D O I
10.1016/j.geosus.2024.01.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Yellow River Basin (YRB) has experienced severe floods and continuous riverbed elevation throughout history. Global climate change has been suggested to be driving a worldwide increase in flooding risk. However, owing to insufficient evidence, the quantitative correlation between flooding and climate change remains illdefined. We present a long time series of maximum flood discharge in the YRB dating back to 1843 compiled from historical documents and instrument measurements. Variations in yearly maximum flood discharge show distinct periods: a dramatic decreasing period from 1843 to 1950, and an oscillating gentle decreasing from 1950 to 2021, with the latter period also showing increasing more extreme floods. A Mann-Kendall test analysis suggests that the latter period can be further split into two distinct sub -periods: an oscillating gentle decreasing period from 1950 to 2000, and a clear recent increasing period from 2000 to 2021. We further predict that climate change will cause an ongoing remarkable increase in future flooding risk and an similar to 44.4 billion US dollars loss of floods in the YRB in 2100.
引用
收藏
页码:193 / 199
页数:7
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