Amplitude and frequency variations of coherent radio signals during probing of the daytime Venusian ionosphere
A. L. Gavrik, Yu. A. Gavrik, T. F. Kopnina, L. N. Samoznaev
Abstract
A. L. Gavrik, Yu. A. Gavrik, T. F. Kopnina, L. N. Samoznaev
Abstract
A new procedure for analyzing the data obtained during radio probing of the Venusian ionosphere is proposed. The experimental results of the two-frequency probing with the use of the “Venera 15” and “Venera 16” orbiters that provide evidence that the daytime Venusian ionosphere has a layered structure are presented. It is shown that there exists a lower part of the daytime ionosphere at altitudes of 80 to 120 km.
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A new procedure for analyzing the data obtained during radio probing of the Venusian ionosphere is proposed. The experimental results of the two-frequency probing with the use of the “Venera 15” and “Venera 16” orbiters that provide evidence that the daytime Venusian ionosphere has a layered structure are presented. It is shown that there exists a lower part of the daytime ionosphere at altitudes of 80 to 120 km.
Key concepts: Daytime, Ionosphere, Venus, Amplitude, Ionospheric propagation, Radio frequency, Geology, Geodesy