A global thermospheric model based on mass spectrometer and incoherent scatter data MSIS. II - Composition

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Atmospheric Composition, Atmospheric Models, Gas Density, Incoherent Scattering, Mass Spectroscopy, Thermosphere, Argon, Diurnal Variations, Helium, Oxygen Atoms, Satellite-Borne Instruments

Scientific paper

Measurements of O, He, and Ar from neutral gas mass spectrometers on four satellites (Ogo 6, San Marco 3, Aeros A, and AEC-C) and inferred oxygen and hydrogen densities from an ion mass spectrometer on AE-C have been combined with a neutral temperature and nitrogen density model to produce a global model of thermospheric composition in terms of inferred variations at 120 km. The data set covers the time period from mid-1969 to mid-1975. The MSIS (mass spectrometer and incoherent scatter data) model is compared with the Ogo 6 model (Hedin et al., 1974). Ar variations at 120 km tend to be in phase with temperature variations and inverse to the He, O, and H variations.

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