Tropical tropospheric ozone observed in Thailand |
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| Institution: | 1. Japan Science and Technology Corporation, 4-1-8, Honcho, Kawaguchi, Saitama 332-0012, Japan;2. Research Center for Advanced Science and Technology, University of Tokyo, 4-6-1, Komaba, Meguro-ku, Tokyo 153-8904, Japan;3. Physics Department, Chiang Mai University, Chiang Mai 50200, Thailand;4. Environmental Research and Training Center, Technopolis, Klong 5, Klong Loung, Phathumthani 12120, Thailand;5. Frontier Research System for Global Change-IGCR Yokohama, 3173-25, Showamachi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan;1. St. Petersburg State University, Institute of Physics, St. Petersburg, Russia;2. Research Institute for Space Medicine Federal Research Clinical Center of Federal Biomedical Agency of Russia, Moscow, Russia;3. Space Climate Research Unit, University of Oulu, Finland;4. State Scientific Center of the Russian Federation Institute of Biomedical Problem of the RAS, Moscow, Russia;1. Medical Laboratories Technology Department, Faculty of Applied Medical Sciences, Taibah University, Madinah, Saudi Arabia;2. Biochemistry Department, Al-Azhar University, Nasr City, Cairo 11751, Egypt;3. Biochemistry and Molecular Medicine Department, College of Medicine, Taibah University, Saudi Arabia;4. Medical Biochemistry Department, Faculty of Medicine, Tanta University, Egypt;5. Clinical Pathology Department, National Cancer Institute, Cairo University, Egypt;6. Pharmacology &Toxicology Department, King AbdulAziz University, Jeddah, Saudi Arabia;1. National Exposure Research Laboratory, Environmental Protection Agency, RTP, NC, USA;2. Office of Air Quality Planning and Standards, U.S. Environmental Protection Agency, RTP, NC, USA |
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| Abstract: | The mixing ratios of surface ozone at two rural/remote sites in Thailand, Inthanon and Srinakarin, have been measured continuously for the first time. Almost identical seasonal variations of O3 with dry season maximum and a wet season minimum with a large seasonal amplitude are observed at both sites during 1996–1998. At Inthanon, the monthly averaged O3 mixing ratios range 9–55 ppb, with the annual average of 27 ppb. The ozone mixing ratios at Srinakarin are in the similar range, 9–45 ppb with annual average of 28 ppb. Based on trajectory analysis of O3 data at Inthanon, the long-range transport of O3 under Asian monsoon regime could primarily explain the low O3 mixing ratios of 13 ppb in clean marine air mass from Indian Ocean during wet season but only partly explain the relatively low O3 mixing ratios, 26 ppb or less, in continental air mass from northeast Asia either in wet or dry season. The highest O3 mixing ratios are found in air masses transported within southeast Asia, averaged 46 ppb in dry season. The high O3 mixing ratios during the dry season are suggested to be significantly due to the local/sub-regional scale O3 production triggered by biomass burning in southeast Asia rather than long-range transport effect. |
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