Retarded lower trace on satellite ionograms as new means for studies of the ionospheric macro-irregularities

Abstract

Experimental data on radio sounding of the ionosphere from satellites at heights below its main maximum are presented. In these data, additional retarded lower trace (RLT) is observed in the ionograms. It is interpreted as a trace of a probing radio signal reflected obliquely from the Earth and coming back to the satellite after refraction by sharp horizontal ionospheric irregularities. Horizontal and vertical cuts of these irregularities as well as the electron-density gradients at their side walls are determined using quantitative methods. Two sequences of ionograms for two adjacent orbits of a satellite are presented and processed for which the critical-frequency maps corrected according to the experiment are constructed. The method of weighted interpolation of approximated values at the adjacent points is used. The horizontal size of the retrieved macroirregularity and the velocity of its motion above the Earth's surface are obtained. A conclusion is drawn that RLT ionograms allow one to diagnose additional parameters of the ionosphere.

Results of ionospheric radio sounding from heights in the vicinity of the F2-layer maximum

“…And also in the diagnosis of large-scale ionospheric inhomogeneities, relating both to the regular structures of the ionosphere (the equatorial anomaly, etc) and to irregular (macro irregularity of seismic origin, etc). In probing the heterogeneity is an ever deeper penetration of radio waves inside the irregularity and, thus, it becomes possible to study the internal structure of these irregularities [3]. The examples of the internal structure of heterogeneities as a regular character, and irregular are presented.…”