Analysis of compound floods from storm surge and extreme precipitation in China

被引:15
作者
Feng, Jianlong [1 ,2 ]
Li, Delei [3 ]
Li, Yanxiao [1 ,2 ]
Zhao, Liang [1 ,2 ]
机构
[1] Tianjin Univ Sci & Technol, Key Lab Marine Resource Chem & Food Technol TUST, Tianjin 300457, Peoples R China
[2] Tianjin Univ Sci & Technol, Coll Marine & Environm Sci, Tianjin 300457, Peoples R China
[3] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
基金
中国国家自然科学基金;
关键词
Compound flood; Storm surge; Extreme precipitation; China; WESTERN NORTH PACIFIC; TROPICAL CYCLONE ACTIVITY; EL-NINO; HEAVY PRECIPITATION; DECADAL OSCILLATION; COASTAL CITY; SALT MARSHES; WATER-LEVEL; RAINFALL; VARIABILITY;
D O I
10.1016/j.jhydrol.2023.130402
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
To enhance flood protection and risk reduction in China's coastal cities, it is crucial to comprehend the variability and underlying causes of compound floods along the coasts arising from storm surges and intense precipitation. The variability of compound floods from storm surge and extreme precipitation from 1958 to 2014 was analyzed using daily maximum sea level data and daily cumulative precipitation from 16 tide gauges along the coast of China. More than 70 % of the storm surges that caused damage from 1989 to 2014 at 14 out of 16 tide gauges were compound floods. We found a strong and seasonally varying dependence between storm surges and extreme precipitation along the coast of China. There were generally positive trends for the annual number of compound events at tide gauges south of 35 degrees N. Compound flood variability was related to large-scale climate modes. The Arctic Oscillation in March was significantly negatively correlated with the compound events at tide gauges north of 35 degrees N, while the opposite was true at tide gauges south of 35 degrees N. The compound events were significantly correlated with the Pacific Decadal Oscillation (PDO) in June at 10 of the 16 tide gauges, and negatively correlated with the Nin similar to o1 + 2 index in February at 7 of the 16 tide gauges. Precipitation extremes determine the changes in the occurrence of compound floods, and by modifying the East Asian summer monsoon and typhoons, the large climate modes are supposed to impact the occurrence of compound floods. Our findings can enhance our understanding of compound floods and provide an important reference for flood risk management, particularly for low-lying coastal cities in China.
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页数:13
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共 102 条
  • [1] Sedimentation rates in flow-restricted and restored salt marshes in Long Island Sound
    Anisfeld, SC
    Tobin, M
    Benoit, G
    [J]. ESTUARIES, 1999, 22 (2A): : 231 - 244
  • [2] Impacts of flow restrictions on salt marshes: An instance of acidification
    Anisfeld, SC
    Benoit, G
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1997, 31 (06) : 1650 - 1657
  • [3] Long term changes in flooding and heavy rainfall associated with North Atlantic tropical cyclones: Roles of the North Atlantic Oscillation and El Nino-Southern Oscillation
    Aryal, Yog N.
    Villarini, Gabriele
    Zhang, Wei
    Vecchi, Gabriel A.
    [J]. JOURNAL OF HYDROLOGY, 2018, 559 : 698 - 710
  • [4] Higher probability of compound flooding from precipitation and storm surge in Europe under anthropogenic climate change
    Bevacqua, E.
    Maraun, D.
    Vousdoukas, M. I.
    Voukouvalas, E.
    Vrac, M.
    Mentaschi, L.
    Widmann, M.
    [J]. SCIENCE ADVANCES, 2019, 5 (09)
  • [5] Caldwell Patrick, 2010, NCEI
  • [6] PDO, ENSO and the early summer monsoon rainfall over south China
    Chan, JCL
    Zhou, W
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (08) : 1 - 5
  • [7] Chang CP, 2001, J CLIMATE, V14, P2376, DOI 10.1175/1520-0442(2001)014<2376:PROACO>2.0.CO
  • [8] 2
  • [9] Tidal Variability Related to Sea Level Variability in the Pacific Ocean
    Devlin, Adam T.
    Jay, David A.
    Zaron, Edward D.
    Talke, Stefan A.
    Pan, Jiayi
    Lin, Hui
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2017, 122 (11) : 8445 - 8463
  • [10] Ding X.L., 2002, J. Geospat. Eng., V4, P41