The O/O2 ratio and eddy mixing at heights from 85 km to the turbopause

Details The O/O2 ratio and eddy mixing at heights from 85 km to the turbopause The O/O2 ratio and eddy mixing at heights from 85 km to the turbopause

Jun 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986jatp...48..563g&link_type=abstract

Journal of Atmospheric and Terrestrial Physics (ISSN 0021-9169), vol. 48, June 1986, p. 563-571.

Physics

Atmospheric Composition, Oxygen, Solar Terrestrial Interactions, Turbopause, Turbulent Diffusion, Vertical Distribution, Annual Variations, Atmospheric Moisture, Diurnal Variations, Geomagnetic Latitude, Photochemical Reactions, Solar Flux

Scientific paper

The O/O2 ratio at heights from 85 km to the turbopause is represented parametrically in terms of eddy diffusion coefficient K, solar dissociating flux, and ambient mesospheric conditions appropriate to a given date and latitude. The relation obtained is consistent with results of detailed calculations undertaken by various authors for the concentration of photochemically produced O under conditions of vertical eddy transport and chemical removal in an otherwise static atmosphere.

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