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).
Similar content being viewed by others
References
N. S. Bakhvalov, Numerical Methods: Analysis, Algebra, Ordinary Differential Equations, (Nauka, Moscow, 1975) [in Russian].
V. Calvert and J. M. Warnok, “Ionospheric Inhomogene-ities Observed during Topside Sounding,” Proc. IEEE 57(6), 182–188 (1969). Equipment for Studying the Topside Ionosphere, (IZMIRAN, Moscow, 1980) [in Russian].
M. D. Fligel’, “On One Possible Mechanism by Which Radiowaves Propagate in the Topside Ionosphere,” Geomagn. Aeron. 29(1), 71–75 (1989).
B. N. Gershman, L. M. Erukhimov, and Yu. Ya. Yashin, Wave Phenomena in the Ionosphere and Space Plasma, (Nauka, Moscow, 1984) [in Russian].
D. C. Jensen and J. C. Cain, “An Interim Geomagnetic Field,” J. Geophys. Res. 67, 3568 (1962).
Yu. A. Kravtsov and Yu. I. Orlov, Ray Optics of Inhomogeneous Mediums, (Nauka, Moscow, 1971) [in Russian]. Proc. IEEE 57 (6) (1969).
Author information
Authors and Affiliations
Additional information
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.
Rights and permissions
About this article
Cite this article
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
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S0016793210010135