Electron-density distributions in the ionosphere derived from propagation measurements made during seven long-range missile flights are given. These results are compared with measurements derived from variable-frequency pulse soundings and with satellite and rocket measurements described by others. The vertical electron-density gradient was found to vary within quite a large range, being lowest for two firings that took place shortly after sunset and greatest for the one early-morning firing. The equilibrium electron-density variation with height was found to be consistent with the assumption of a Chapman layer, of varying scale height, based on a recent model of the neutral atmosphere derived from satellite retardation measurements.
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Nisbet et al. (1960) studied this question.
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