RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2022, Vol. 31 >> Issue (5): 1169-1185.doi: 10.11870/cjlyzyyhj202205019

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Scavenging Effect of Different Types of Rainfall on  PM2.5 in Main Urban Area of Chongqing
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CHEN Xiao-min1, ZOU Qian2,YANG Le1,FU Ju1, LIAO Xiao-li1   

  1. (1.Chongqing Weather Modification Office, Chongqing 401147,China;2. Chongqing Meteorological Observatory, Chongqing 4401147,China)
  • Online:2022-05-20 Published:2022-06-02

Abstract: Because of complex underlying surface, low surface wind and high air humidity, which are easy to cause the accumulation of PM2.5 in main urban area of Chongqing, Precipitation play an important role in PM2.5 removal by the scavenging effect. Based on the meteorological observation data at Shapingba station and the hourly PM2.5 mass concentration observation data in main urban area of Chongqing from 2015-2020, the scavenging effect of different type of rainfall processes on PM2.5 mass concentration is analyzed. The results showed that: In the threshold analysis of PM2.5 mass concentration in different rainfall processes, the initial mass concentration is the main influencing factor. Both rainfall processes with cold front and strong rainfall with no(weak)cold air can effectively reduce PM2.5 mass concentration. In weak rainfall processes with no(weak)cold air, rainfall erosion and the hygroscopic growth of PM2.5 make the PM2.5 mass concentration change smaller. Cold front rainfall process average scavenging rate is higher than rainfall process with no(weak)cold air 1-2 grades, The average scavenging rate of rainfall process with no(weak)cold air increases with the increase of hourly maximum rainfall intensity, rainfall duration and accumulated rainfall. and the PM2.5 mass concentration can be reduced by about 1/4 in the convective rainfall process of 3 h or more. The raindrop spectrum in the central urban area of Chongqing conforms to Gamma distribution, and there is little difference in the scavenging coefficient of aerosol particles in different spectral types of stable rainfall. The scavenging coefficient of aerosol particles in convective rainfall with maximum hourly rainfall ≥20 mm is significantly higher than that of other convective rainfall.

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