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Данилкин, Н. П.; Kotonaeva, N. G.

doi:10.1023/a:1019648108571

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Calculation Of the Electron-density Profile By Ionospheric R1

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2009

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Cited by 2 publications

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“…For retrieval of the profile by the trace of the ordinary component, one can make use of both one of the methods of solution of the inverse problem, in which the true height of reflection from the ionosphere is found by the effective height (e.g., Titeridge's method; its description and application to ionograms from the "Mir" space station are given in the previous publications [4]) and the method of successive approximation for solution of the direct problem.…”

Section: Calculation Of the Electron-density Profile By Ionospheric Rmentioning

confidence: 99%

Z component of a magnetically split signal used for ionospheric radio sounding from the vicinity of the F2-layer maximum

Kotonaeva

2009

Radiophys Quantum El

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The radio signal radiated and propagated in a plasma has two modes of the extraordinary component, x and z. When the radio sounding is performed from altitudes more than 500 km, the z component ceases to exist at altitudes greater than the altitude of the F 2 -layer maximum. However, the z component reaches these altitudes during sounding from the vicinity of the main maximum of the electron density. We study the behavior of the z component when the signal source is located at different altitudes in the ionosphere and also consider the capabilities and method of calculation of the plasma-frequency altitude profile by the z-component trace in ionograms.

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Section: Calculation Of the Electron-density Profile By Ionospheric Rmentioning

confidence: 99%