Negative ions in the lower atmosphere
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概要
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The chemical compositions of negative ions in the lower atmosphere (0-30km altitude) at middle latitudes were investigated with two models, one for the lower stratosphere (15-30km) and the other for the troposphere (0-15km). The calculated result shows that the predominant ion species are NO_3^-HNO_3H_2O in the height range of 0-10km and NO_3^-(HNO_3)_2 in 10-30km, and other main negative species have NO_3^- or HSO_4^- cores. In general, the calculated result agrees with the observed one. A possible role of the ions and aerosols generated by the ion-nucleation mechanism is suggested for the Antarctic springtime 'ozone hole' phenomenon.
- 国立極地研究所の論文
著者
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Ogawa Toshio
Department Of Electronic Engineering Shizuoka Institute Of Science And Technology
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Ogawa Toshio
Department Of Physics Faculty Of Science Kochi University
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Kawamoto Hiroto
Department of Physics, Faculty of Science, Kochi University
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Kawamoto Hiroto
Department Of Physics Faculty Of Science Kochi University
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Ogawa Toshio
Department of Electrical and Electronic Engineering, Faculty of Science and Technology, Shizuoka Institute of Science and Technology, 2200-2 Toyosawa, Fukuroi, Shizuoka 437-8555, Japan
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Ogawa Toshio
Department of Chemistry, College of General Education, Nagoya University
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