Several notes on the OH* layer
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Date
2015
Authors
Volume
33
Issue
7
Journal
Annales geophysicae
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Publisher
Katlenburg, Lindau : Copernicus
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Abstract
This brief note introduces several analytical approaches to OH* layer parameters. The number density and height of the OH* layer peak are determined by the distributions of atomic oxygen and temperature, and by corresponding vertical gradients. The theory can be applied to satellite-borne and ground-based airglow measurements, as well as to model results.
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CC BY 3.0 Unported