A Temporal Increase in the Atmospheric 210Pb Concentration Possibly Due to the 1991 Eruption of Pinatubo Volcano
Author:
Affiliation:
1. Department of Industrial Chemistry, School of Science and Technology, Meiji University
2. National Institute for Environmental Studies
Publisher
Japan Radioisotope Association
Subject
Radiation
Link
https://www.jstage.jst.go.jp/article/radioisotopes1952/48/8/48_8_522/_pdf
Reference39 articles.
1. 1) Brewer, A. W.: Evidence for a world circulation provided by the measurements of helium and water vapour distribution in the stratosphere, Quart. J. Roy. Met. Soc. Lond., 75, 351-363 (1949)
2. 2) Shimazaki, T.: “Seisoken ozon (Stratospheric ozone) ”, 2nd ed., p. 129, Univ. Tokyo Press, Tokyo (1989) (in Japanese)
3. 3) Berggren, R. and Labitzke, K.: A detailed study of the horizontal and vertical distribution of ozone, Tellus, 18, 761-772 (1966)
4. 4) Feely, H. W. and Seitz, H.: Use of lead 210 as a tracer of transport processes in the stratosphere, J. Geophys. Res., 75, 2885-2894 (1970)
5. 5) Moore, H. E., Poet, S. E. and Martell, E. A.: 222Rn, 210Pb, 210Bi, and 210Po profiles and aerosol residence times versus altitude, J. Geophys. Res., 78, 7065-7075 (1973)
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