长江流域资源与环境 >> 2022, Vol. 31 >> Issue (5): 1169-1185.doi: 10.11870/cjlyzyyhj202205019

• 生态环境 • 上一篇    

重庆中心城区不同类型降雨对PM2.5清除作用分析

陈小敏1, 邹倩2,杨乐1, 付驹1, 廖晓荔1   

  1. (1.重庆市人工影响天气办公室,重庆 401147;2.重庆市气象台,重庆 401147)

  • 出版日期:2022-05-20 发布日期:2022-06-02

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

摘要: 重庆中心城区下垫面复杂,地面风速小,湿度大,易造成PM2.5在本地累积增长,降雨的冲刷和清除对降低PM2.5质量浓度起着重要作用。利用2015~2020年沙坪坝站雨量、雨滴谱观测资料和重庆主城区小时PM2.5质量浓度观测数据,分析了不同类型降雨过程对PM2.5质量浓度的影响。结果表明:不同类型降雨过程对PM2.5质量浓度影响的阈值分析中,初始质量浓度都是的主要影响因素。 显著冷空气降雨过程和无(弱)冷空气较强降雨过程都能有效降低 PM2.5质量浓度,无(弱)冷空气弱降雨过程中,降雨冲刷和PM2.5的吸湿性增长共同作用使得PM2.5质量浓度变化幅度较小。显著冷空气降雨过程平均清除率比无(弱)冷空气降雨过程高1~2个等级,无(弱)冷空气降雨过程平均清除率随小时最大雨量、降雨时长和累积雨量的增加而增大,3 h及以上的对流性降雨过程可使PM2.5质量浓度降低约1/4。重庆中心城区降雨雨滴谱符合Gamma分布,稳定性降雨不同谱型雨滴对各粒径气溶胶粒子清除系数差别较小,小时最大雨量≥20 mm的对流性降雨中雨滴对各粒径气溶胶粒子的清除系数明显高于其它等级对流性降雨。

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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