Solar flux variation of the thermospheric molecular oxygen density
1980
Measurements of the thermospheric molecular oxygen density obtained from the Atmosphere Explorer (AE) satellites and composition data obtained previously from rocket-based experiments provide complimentary information on the distribution of O2 between 120 and 200 km as a function of solar flux. The AE measurements provide a description of the constituent's short-term behavior near solar minimum. With this knowledge, the rocket experiment data, which cover a wider range of solar activity and altitudes, can be analyzed for long-term variations. At mid-latitudes and low latitudes the 200-km O2/N2 density ratio decreases ∼35% as the F10.7 index increases from 70 to 150. The O2 density at 200 km shows little variation but at 120 km decreases ∼30% for the same increase in F10.7. Additionally, the analysis gives evidence for photochemically induced departures from diffusive equilibrium in the molecular oxygen density.
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