Effects of urbanization on extreme precipitation based on Weather Research and Forecasting model: A case study of heavy rainfall in Beijing

被引:0
|
作者
Pei, Yujia [1 ,2 ]
Liu, Jiahong [1 ,2 ,3 ]
Wang, Jia [2 ,3 ]
Mei, Chao [2 ,3 ]
Dong, Lirong [1 ,2 ]
Wang, Hao [2 ,3 ]
机构
[1] Beijing Univ Technol, Fac Architecture Civil & Transportat Engn, Beijing 100124, Peoples R China
[2] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China
[3] Minist Water Resources, Key Lab River Basin Digital Twinning, Beijing 100038, Peoples R China
基金
中国国家自然科学基金; 北京市自然科学基金;
关键词
Extreme precipitation; The "23.7" storm; Beijing; WRF; Urbanization; PEARL RIVER DELTA; SIMULATION; PARAMETERIZATION; IMPACT;
D O I
10.1016/j.ejrh.2024.102078
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study Region: Beijing Study focus: Urbanization has altered the processes of the hydrological cycle in cities, further affecting their precipitation extremes. This study utilizes Weather Research and Forecasting model (WRF) to investigate the sensitivity of extreme precipitation to urbanization, exemplified by analyzing the "23.7" extraordinary rainstorm in Beijing.Two comparative urban development scenarios (1980 and 2020) were designed, using the real underlying surface as the static geographic data for the WRF model. Furthermore, the reliability of the model results was validated through an analysis of the extreme precipitation event that occurred in July 2021, reinforcing the findings of this study. New Hydrological Insights for the Region: The simulated precipitation is well represented by using the underlying surface data post-urbanization. Furthermore, the study reveals that urbanization has augmented the total rainfall of two extreme precipitation events in Beijing: the "23.7" event and the event on July 12, 2021. Specifically, there was an increase of 19.1 mm and 7.1 mm, respectively, in the rainfall within the core urban area during these two extreme precipitation events, when comparing the underlying surface scenarios from 1980 to 2020. Analyzing the impact mechanism, weakened horizontal winds in the urban core prolong water vapor residence, altering land surface energy balance to boost temperature and convection, both contributing to urban-induced precipitation increase.
引用
收藏
页数:15
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