2006년 4월 안면도에서 발생한 황사, 안개, 청명, 구름 사례에 대한 에어러솔 특성 분석

A case study of aerosol features of Asian dust, fog, clear sky, and cloud at Anmyeon Island in April 2006

  • 구태영 (기상청 기후변화감시센터) ;
  • 홍기만 (기상청 기후변화감시센터) ;
  • 김상백 (기상청 기후변화과학대책과) ;
  • 공종웅 (기상청 기후변화감시센터) ;
  • 김명수 (기상청 기후변화감시센터)
  • Goo, Tae-Young (Korea Global Atmosphere Watch Center, Korea Meteorological Administration) ;
  • Hong, Gi-Man (Korea Global Atmosphere Watch Center, Korea Meteorological Administration) ;
  • Kim, Sang-Beak (Climate Change Science Program Division, Korea Meteorological Administration) ;
  • Gong, Jong-Ung (Korea Global Atmosphere Watch Center, Korea Meteorological Administration) ;
  • Kim, Myoung-Soo (Korea Global Atmosphere Watch Center, Korea Meteorological Administration)
  • 투고 : 2007.12.25
  • 심사 : 2008.04.21
  • 발행 : 2008.06.01

초록

The aerosol characteristics in terms of 4 different cases (Asian dust, fog, clear sky and cloud) which had happened at Anmyeon Island in April 2006 were studied using various measurements such as the Micro Pulse Lidar (MPL), sunphotometer, $\beta$-ray $PM_{10}$ Analyzer, anemoscope and anemometer. In addition, synoptic charts, back trajectory analyses and satellite images were also used to help characterize the aerosol events. The aerosol optical properties were featured by the Aerosol Optical Depth (AOD) and ${\AA}ngstr\ddot{o}m$ exponent which were estimated by the sunphotometer. When Anmyeon Island was dominated by the Asian dust, the AOD was sharply increased as seven times as a yearly average of it (0.35). As compared with a yearly average of the ${\AA}ngstr\ddot{o}m$ exponent of 0.97, the ${\AA}ngstr\ddot{o}m$ exponent of a dust day was significantly low (0.099). In addition, $PM_{10}$ mass concentration showed an extremely high record. The maximum concentration reached $1790.5{\mu}gm^{-3}$ on 8 April 2006. The maximum mass concentration was shown with delay when the wind speed of $0ms^{-1}$ was observed. It was also found that a satellite image of the MODIS-RGB had a good agreement with the results of those measurements. It was shown that the MPL was able to describe effectively the vertical distribution of aerosol for all the cases. In particular, the MPL evidently captured the aerosol layer before the cloud observation. The aerosol layer was similarly described by the AOD. On a clear sky day, the AOD had not only a very low value (0.054) but also a feature of homogeneity.

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