Peculiarities of the lower thermosphere composition variations at high latitudes from the results of rocket experiments

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Atmospheric Composition, Auroras, Ionospheric Composition, Magnetic Storms, Rocket Sounding, Thermosphere, Argon, Correlation Coefficients, Kp Index, Magnetosphere-Ionosphere Coupling, Nitrogen, Oxygen Atoms

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An analysis of the results of more than 50 rocket experiments on the measurement of the thermosphere composition at 120-160 km height carried out during 1968-1989 (February, March) on the Heyss Island (80 deg 37 N 58 deg E) has been conducted. During the development of the magnetosphere substorm the decrease of O/N2, O/Ar ratios in the morning and evening sectors of the auroral oval and their increase in the polar cap take place. Correlation coefficients of O/N2 with Kp for the auroral oval zone and the polar cap correspondingly are equal to -0.8 and +0.6 at the 115 km height. The latter effect is attributed to the observed increase of O/N2, this corresponds to the thermosphere adiabatic cooling in the night sector of the polar cap, which evidently acts jointly with the vertical transport effects.

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