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New indices for wet scavenging of air pollutants (O-3, CO, NO2, SO2, and PM10) by summertime rain

  • Yoo, Jung-Moon (유정문, Dept. of Science Education, Ewha Womans University, Seoul, Republic of Korea) , Lee, Yu-Ri (Dept. of Atmospheric Sciences, Yonsei University, Seoul, Republic of Korea) , Kim, Dongchul (Universities Space Research Association, Columbia, MD, USA, NASA/Goddard Space Flight Center, Greenbelt, MD, USA) , Jeong, Myeong-Jae (Dept. of Atmospheric and Environmental Sciences, Gangneung-Wonju National University, Gangneung, Republic of Korea) , Stockwell, William R. (Dept. of Chemistry, Howard University, Washington, DC, USA) , Kundu, Praun K. (JCET, University of Maryland Baltimore County, Baltimore, MD, USA, NASA/Goddard Space Flight Center, Greenbelt, MD, USA) , Oh, Soo-Min (Dept. of Science Education, Ewha Womans University, Seoul, Republic of Korea) , Shin, Dong-Bin (Dept. of Atmospheric Sciences, Yonsei University, Seoul, Republic of Korea) , Lee, Suk-Jo (National Institute of Environmental Research, Inchon, Republic of Korea)
  • ATMOSPHERIC ENVIRONMENT[1352-2310], 2014, v.82, 226-237

초록/요약

The washout effect of summertime rain on surface air pollutants (O-3, CO, NO2, SO2, and PM10) has been investigated over South Korea during 2002-2012 using routinely available air-monitored and meteorological data. Three new washout indices for PM10, SO2, NO2, and CO are developed to express the effect of precipitation scavenging on these pollutants. All of these pollutants show statistically significant negative correlations between their concentrations and rain intensity due to washout or convection. The washout effect is estimated for precipitation episodes classified by rain intensity (one set included all episodes and another included a subset of moderate intensity episodes that exclude Changma and typhoons), based on the log-transformed hourly data. The most sensitive air pollutant to the rain onset among these five air pollutants is PM10. The relative effect of the rainfall washout on the air pollutant concentrations is estimated to be: PM10 > SO2 > NO2 > CO > O-3, indicating that PINAio is most effectively scavenged by rainfall. The analysis suggests that the O-3 concentrations may increase due to vertical mixing leading to its downward transport from the lower stratospherelupper troposphere. The concentrations of CO are reduced, probably due to both the washout and convection. The concentrations of NO2 are affected by the opposing influences of lightning-generation and washout and this are discussed as well. (C) 2013 The Authors. Published by Elsevier Ltd. All rights reserved.

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