The diurnal and solar cycle variation of the charge exchange induced hydrogen escape flux

Physics

Scientific paper

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Charge Exchange, Diurnal Variations, Hydrogen Atoms, Solar Cycles, Electron Energy, Ion Density (Concentration), Ion Temperature, Ogo-6, Solar Activity Effects

Scientific paper

On the basis of ion temperature and density data at specific points and times in June 1969 provided by the OGO 6 satellite, and altitude profiles of the ion and electron temperature and concentration provided by the Arecibo radar facility over the period February 1972-April 1974, the diurnal and solar cycle variation of the charge-exchange-induced hydrogen escape flux was investigated. It was calculated that for low to moderate solar activity at Arecibo, the diurnal ratio of the maximum-to-minimum charge-exchange-induced hydrogen escape flux was approximately 6 with a peak around noon and a minimum somewhere between 0100 and 0300 h LT. This study of a limited amount of OGO 6 and Arecibo data seems to indicate that the charge-exchange-induced hydrogen escape flux increases as the F(10.7) flux increases for low to moderate solar activity.

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