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GOCI 자료를 이용한 서울 지역 고농도 미세먼지와 옅은 황사 시 에어로졸 광학적 특성 분석

Analysis of Aerosol Optical Properties for High Particulate Matters and Light Asian Dust in Seoul Using GOCI

  • 김덕래 (국립환경과학원 기후대기연구부 지구환경연구과) ;
  • 최원준 (국립환경과학원 기후대기연구부 지구환경연구과) ;
  • 최명제 (연세대학교 대기과학과) ;
  • 김지영 (국립환경과학원 기후대기연구부 지구환경연구과) ;
  • 조아라 (국립환경과학원 기후대기연구부 지구환경연구과) ;
  • 김상균 (국립환경과학원 기후대기연구부 지구환경연구과) ;
  • 김준 (연세대학교 대기과학과) ;
  • 문경정 (국립환경과학원 기후대기연구부 지구환경연구과)
  • Kim, Deok-Rae (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research) ;
  • Choi, Won-Jun (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research) ;
  • Choi, Myungje (Department of Atmospheric Sciences, Yonsei University) ;
  • Kim, Jiyoung (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research) ;
  • Cho, Ara (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research) ;
  • Kim, Sang-Kyun (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research) ;
  • Kim, Jhoon (Department of Atmospheric Sciences, Yonsei University) ;
  • Moon, Kyung-Jung (Global Environment Research Division, Climate and Air Quality Research Department, National Institute of Environmental Research)
  • 투고 : 2017.02.24
  • 심사 : 2017.04.13
  • 발행 : 2017.06.30

초록

To distinguish between high particulate matter (HPM) and light Asian dust (LAD) events, aerosol optical properties from GOCI were investigated in Seoul from 2014 to 2016. The poor air quality case caused by fine atmospheric particulate matter (i.e., 80<$PM_{10}$<$400{\mu}g/m^3$) is clearly separated from the case of heavy Asian dust that generally shows the $PM_{10}$ concentration more than $400{\mu}g/m^3$. In this study, we have found eight cases for the poor air quality and divided them into the two events(i.e., HPM and LAD). In case of aerosol optical depth (AOD), there was no big difference between two events. However, Angstrom exponent (AE) for HPM events was greater than 1, while that for LAD events less than 1. As a result of comparing aerosol type, non-absorbing fine mode aerosols were dominant for HPM events, but coarse and absorbing coarse mode aerosols for LAD events. Therefore, AE and aerosol type from GOCI can be used to distinguish between two events effectively.

키워드

참고문헌

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