By P. M. Banks and G. Kockarts (Auth.)
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Hanel, V. G. Kunde, and C. Prabhakara, /. Geophys. Res. 75, 5831 (1970). 1 Introduction The transition from the homosphere to the heterosphere involves a competition between mixing and diffusive processes. The former tends to keep the mean molecular mass constant with altitude, while the latter acts to let each gas constituent assume a density and pressure distribution consistent with its own mass and temperature. In the case of the earth's atmosphere there is an additional complication which arises from the photodissociation of molecular oxygen.
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