Reconstruction of Electron-Density Height Profiles Based in the Bottomside Ionosphere on Topside Satellite Sounding Data with the IRI Model

• Published in: Geomagnetism and Aeronomy Vol. 61; no. 2; pp. 241 - 258
• Main Authors: Denisenko, P. F., Sotsky, V. V.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01.03.2021; Springer Nature B.V
• Subjects: E region; Earth and Environmental Science; Earth Sciences; Earth surface; Electron density; F 2 region; F region; Geophysics/Geodesy; Ionograms; Ionosphere; Mathematical models; Optimization; Parameters; Reconstruction; Satellite sounding; Satellites; Sounding
• ISSN: 0016-7932; 1555-645X; 0016-7940
• DOI: 10.1134/S0016793221020067

A method is proposed to determine the total height profiles of the electron density in the ionosphere with the use of topside satellite ionograms containing traces of sounding signal reflections from the Earth’s surface. The monotonic profile from the satellite to a certain height hm above the height hmF 2 of the F 2-layer maximum is calculated with the classical method based on reflections from the topside ionosphere. Below the height hm , down to the ionospheric base, the profile is represented by a system of interrelated analytical functions with a limited number of parameters. Their values are found with optimization methods and the joint use of traces of signal reflections, both from the outer part of the ionosphere and from the Earth. To increase the stability of the problem, the lower part of the sought profile in the E region is specified by an unchangeable profile from the IRI-2016 model. The method reliably determines the parameters of the hmF 2 maximum, NmF 2, and the profile in its vicinity. The addition of key parameters— hmF 2, NmF 2, and the additionally calculated values B 0 and B 1, which determine the profile shape in the F region—to the IRI model makes it possible to obtain an IRI profile that is corrected for the actual experimental conditions. The calculated and corrected profiles are similar in the bottomside ionosphere and can noticeably differ in the topside ionosphere. Thus, the use of this proposed method for the reconstruction of the total height profile of the electron density expands the informational value of topside satellite sounding of the ionosphere.