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Science 13 January 1967:
Vol. 155. no. 3759, p. 189
DOI: 10.1126/science.155.3759.189

Articles

Volcanic Sunset-Glow Stratum: Origin

A. B. Meinel 1 and M. P. Meinel 1

1 Steward Observatory, University of Arizona, Tucson 85721

Reexamination of the phenomenon of volcanic-dust sunsets, as typified by the Krakatoa event, supports a theory that the scattering layer is produced by the interaction of ozone and sulfur dioxide in much the same manner as is the normal "Junge"aerosol layer at 20 kilometers.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Organogenic Dolomitization in Peritidal to Deep-Sea Sediments.
(2000)
Journal of Sedimentary Research 70, 10-23
Coastal upwelling and a history of organic-rich mudstone deposition off Peru.
E. Suess, L. D. Kulm, and J. S. Killingley (1987)
Geological Society, London, Special Publications 26, 181-197
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Trajectory of the Mt. St. Augustine 1976 Eruption Ash Cloud.
A. B. Meinel, A. B. MEINEL, M. P. MEINEL, and G. E. SHAW (1976)
Science 193, 420-422
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Stratospheric Dust-Aerosol Event of November 1974.
A. B. Meinel, A. B. Meinel, and M. P. Meinel (1975)
Science 188, 477-478
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