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Specific propagation of radiowaves from the Intercosmos-19 satellite in the region of the nighttime equatorial anomaly crest

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Abstract

It has been indicated how a complex ionogram of topside sounding near the outer slope of the winter southern crest of the equatorial anomaly, where a large NmF2, gradient and a deep hmF2, minimum are observed, is formed. The model latitudinal cross-sectio n of the ionosphere, used to perform trajectory calculations, has been constructed based on the corrected Intercosmos-19 data. The ray trajectories have been modeled using the method of characteristics. It has been indicated that a complex Intercosmos-19 ionogram is formed by an oblique reflection from the equatorial anomaly crest slope (the main trace) and by a strongly oblique reflection from the crest bottom as a result of the wave capture by a large-scale inhomogeneity (the additional trace).

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Original Russian Text © G.A. Zhbankov, A.T. Karpachev, V.A. Telegin, K.G. Tsybulya, 2010, published in Geomagnetizm i Aeronomiya, 2010, Vol. 50, No. 1, pp. 123–130.

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Zhbankov, G.A., Karpachev, A.T., Telegin, V.A. et al. Specific propagation of radiowaves from the Intercosmos-19 satellite in the region of the nighttime equatorial anomaly crest. Geomagn. Aeron. 50, 119–126 (2010). https://doi.org/10.1134/S0016793210010135

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  • DOI: https://doi.org/10.1134/S0016793210010135

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