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Articles
Volcanic Sunset-Glow Stratum: Origin
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.
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Science. ISSN 0036-8075 (print), 1095-9203 (online)