4.7 Article

New indices for wet scavenging of air pollutants (O3, CO, NO2, SO2, and PM10) by summertime rain

Journal

ATMOSPHERIC ENVIRONMENT
Volume 82, Issue -, Pages 226-237

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2013.10.022

Keywords

Air pollutants; Washout; Rainfall; Surface measurement over South Korea; Statistical significance

Funding

  1. National Research Foundation of Korea (NRF) [2009-0083527]
  2. Korean Ministry of Environment [201200016003]
  3. National Oceanic and Atmospheric Administration
  4. National Aeronautics and Space Administration
  5. Korea Environmental Industry & Technology Institute (KEITI) [ARQ201204017003] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  6. National Research Foundation of Korea [2009-0083527] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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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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