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인공위성 (SCIAMACHY) 데이터를 이용한 대류권 SO2, NO2 측정: 2006년 동북아시아 지역의 계절적 SO2, NO2 변화 추세
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  • 인공위성 (SCIAMACHY) 데이터를 이용한 대류권 SO2, NO2 측정: 2006년 동북아시아 지역의 계절적 SO2, NO2 변화 추세
저자명
이철규,김영준,Lee. Chul-Kyu,Kim. Young-J.
간행물명
한국대기환경학회지
권/호정보
2008년|24권 2호|pp.176-188 (13 pages)
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한국대기환경학회
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이 논문은 한국과학기술정보연구원과 논문 연계를 통해 무료로 제공되는 원문입니다.
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기타언어초록

Anthropogenic emissions of nitrogen oxides and sulfur dioxide in Northeast Asia are of great concern because of their impact on air quality and atmospheric chemistry on regional and intercontinental scales. Satellite remote sensing based on DOAS (Differential Optical Absorption Spectroscopy) technique has been preferred to measure atmospheric trace species and to investigate their emission characteristics on regional and global scales. Absorption spectra obtained by the satellite-born instrument, SCIAMACHY (Scanning Imaging Absorption Spectrometer for Atmospheric Chartography) have been utilized to retrieve the information of $SO_2$ and $NO_2$ over Northeast Asia. $SO_2$ levels over Northeast Asia were in order of East China, Yellow Sea, South Sea and Korean Peninsula with mean vertical columns of $1.78({pm}1.0){ imes}10^{16}$, $1.11({pm}0.67){ imes}10^{16}$, $0.60({pm}0.63){ imes}10^{16}$, $0.71({pm}0.65){ imes}10^{16};molecules/cm^2$, respectively. $NO_2$ levels were in order of East China, Yellow Sea, Korean Peninsula, and South Sea with mean vertical columns of $1.2({pm}0.56){ imes}10^{16}$, $0.38({pm}0.19){ imes}10^{16}$, $0.48({pm}0.28){ imes}10^{16}$, $0.26({pm}0.16){ imes}10^{16};molecules/cm^2$, respectively. High levels of $SO_2$ and $NO_2$ were observed over East China, in particular in winter by the contribution of heating fuel combustion exhausts. The $SO_2$ and $NO_2$ levels over East China were the highest in January with 34% and 42% higher over the annual means. Low levels of $SO_2$ ranged over Korean peninsula, while $NO_2$ levels were relatively high, in particular in winter. The $SO_2$ and $NO_2$ levels over Yellow Sea were relatively higher compared to those over Korean peninsula and South Sea, which could be mainly attributed to their transport from East China.