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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

Postal Subscription Code 80-963

2018 Impact Factor: 1.205

Front. Earth Sci.    2018, Vol. 12 Issue (4) : 834-845    https://doi.org/10.1007/s11707-018-0730-z
RESEARCH ARTICLE
A study on flooding scenario simulation of future extreme precipitation in Shanghai
Xiaoting WANG, Zhan’e YIN(), Xuan WANG, Pengfei TIAN, Yonghua HUANG
Department of Geography, Shanghai Normal University, Shanghai 200234, China
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Abstract

In the context of climate warming and urbanization, predictions and inundation simulations for future extreme precipitation have become highly active research topics. In this paper, using daily precipitation recorded at 10 meteorological stations in Shanghai for the period 1961–2010, the daily precipitation of each station during the period 2011–2099 was simulated by the statistical downscaling model (SDSM). And we examined the varying tendencies of future precipitation by the Mann-Kendall test. Further, the Soil Conservation Service (SCS) model and Pearson-III distribution curve were used to simulate the waterlogging duration and depth of future extreme precipitation in different scenarios with 3-, 5-, 10-, 20-, 50-, and 100-year return periods. The results show that: 1) Precipitation in Shanghai before the 2050s shows a trend of increasing and decreasing alternations, followed by a trend of decreasing and a marked decrease in about the 2070s. 2) In the 21st century, the waterlogging duration with return periods of 3, 5, and 10 years in Shanghai is predicted to last for less than 30 minutes, while the return periods of 20, 50, and 100 years last for less than 45 minutes. From the spatial distribution, the waterlogging duration to the east and south of the Huangpu River is predicted to be shorter than that of the west and north. 3) With the increase of the return periods, the depth of waterlogging is predicted to increase. The deepest inundated areas are Jinshan to the south-west of Shanghai, the east side of the Huangpu River, and Chongming Island.

Keywords flooding scenario simulation      future extreme precipitation      Shanghai     
Corresponding Author(s): Zhan’e YIN   
Just Accepted Date: 12 October 2018   Online First Date: 07 November 2018    Issue Date: 20 November 2018
 Cite this article:   
Xiaoting WANG,Zhan’e YIN,Xuan WANG, et al. A study on flooding scenario simulation of future extreme precipitation in Shanghai[J]. Front. Earth Sci., 2018, 12(4): 834-845.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-018-0730-z
https://academic.hep.com.cn/fesci/EN/Y2018/V12/I4/834
Fig.1  The spatial distribution of 10 weather stations across Shanghai.
Land type Curve number
Water 100
Park 70
Forestland 57
Green space 62
Unused land 83
Natural village 76
Old residential 92
Cultivated land 78
Public building 88
Warehouse land 89
New residential 86
Roads and squares 98
Commercial and industrial 93
Tab.1  CN values in SCS model
Forecast volume Forecast factor
Precipitation r500 (relative humidity at 500 hPa)
r850 (relative humidity at 850 hPa)
p8_v (convective velocity at 850 hPa)
p8_z (vortices at 850 hPa)
Tab.2  Predictor screening results
Precipitation station Correlation coefficient (r)
Xujiahui 0.68
Minhang 0.71
Baoshan 0.72
Jiading 0.75
Chongming 0.77
Nanhui 0.79
Jinshan 0.74
Qingpu 0.73
Songjiang 0.74
Fengxian 0.71
Tab.3  Coefficient of association (SDSM)
Fig.2  Trend analysis of future precipitation amounts.
Fig.3  Waterlogging duration in the first half of the 21st century under different return periods.
Fig.4  Waterlogging depth in the first half of the 21st century under different return periods (left 15 minutes, right 30 minutes).
Fig.5  Waterlogging duration in the second half of the 21st century under different return periods.
Fig.6  Waterlogging depth in the second half of the 21st century under different return periods (left 15 minutes, right 30 minutes).
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