Estimate of the effects of Pinatubo eruption in stratospheric O3 and NO2 contents taking into account the variations in the solar activity
Author:
Publisher
Pleiades Publishing Ltd
Subject
Atmospheric Science,Earth-Surface Processes,Atomic and Molecular Physics, and Optics,Oceanography
Link
http://link.springer.com/content/pdf/10.1134/S102485601405008X.pdf
Reference28 articles.
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3. S. Chandra, “Changes in stratospheric ozone and temperature due to the eruption of Mt. Pinatubo,” Geophys. Rev. Lett. 20(1), 33–36 (1993).
4. D. J. Hofmann, S. J. Oltmans, W. D. Komhyr, J. M. Harris, J. A. Lathrop, A. O. Langford, T. Deshler, B. J. Johnson, A. Torress, and W. A. Matthews, “Ozone loss in the lower stratosphere over the United States in 1992–1993: Evidence for heterogeneous chemistry on the Pinatubo aerosol,” Geophys. Rev. Lett. 21(1), 65–68 (1994).
5. W. B. Grant, E. V. Browell, J. Fishman, V. J. Brackett, R. E. Veiga, D. Nganga, A. Minga, B. Cros, C. F. Butler, M. A. Fenn, C. S. Long, and L. L. Stowe, “Aerosol-associated changes in tropical stratospheric ozone following the eruption of Mount Pinatubo,” J. Geophys. Res., D 99(4), 8197–8211 (1994).
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