Tropical tropospheric ozone observed in Thailand

被引:60
作者
Pochanart, P
Kreasuwun, J
Sukasem, P
Geeratithadaniyom, W
Tabucanon, MS
Hirokawa, J
Kajii, Y
Akimoto, H
机构
[1] Japan Sci & Technol Corp, Kawaguchi, Saitama 3320012, Japan
[2] Univ Tokyo, Adv Sci & Technol Res Ctr, Meguro Ku, Tokyo 1538904, Japan
[3] Chiang Mai Univ, Dept Phys, Chiang Mai 50200, Thailand
[4] Technopolis, Environm Res & Training Ctr, Klong Loung 12120, Phathumthani, Thailand
[5] IGCR Yokohama, Frontier Res Syst Global Change, Kanazawa Ku, Yokohama, Kanagawa 2360001, Japan
关键词
biomass burning; regional source; southeast Asia; trajectory analysis; long-range transport;
D O I
10.1016/S1352-2310(00)00441-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 O-3 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 O-3 mixing ratios range 9-55 ppb, with the annual average of 27 ppb. The ozone mixing ratios at Srinakarin are in the similar ranger 9-45 ppb with annual average of 28 ppb. Based on trajectory analysis of O-3 data at Inthanon, the long-range transport of O-3 under Asian monsoon regime could primarily explain the low O-3 mixing ratios of 13 ppb in clean marine air mass From Indian Ocean during Wet season but only partly explain the relatively low O-3 mixing ratios, 26 ppb or less, in continental air mass From northeast Asia either in wet or dry season. The highest O-3 mixing ratios are found in air masses transported within southeast Asia, averaged 46 ppb in dry season. The high O-3 mixing ratios during the dry season are suggested to be significantly due to the local/sub-regional scale O-3 production triggered by biomass burning in southeast Asia rather than long-range transport effect. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:2657 / 2668
页数:12
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