Faraday polarization fluctuations of transionospheric propagation

Details Faraday polarization fluctuations of transionospheric propagation Faraday polarization fluctuations of transionospheric propagation

Feb 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982jgr....87..751l&link_type=abstract

Journal of Geophysical Research, vol. 87, Feb. 1, 1982, p. 751-755.

Physics

2

Beacon Satellites, Faraday Effect, Ionospheric Propagation, Polarized Electromagnetic Radiation, High Frequencies, Power Spectra, Time Response, Very High Frequencies

Scientific paper

Single wave scattering from ionospheric irregularities is used to study rapid, intense Faraday polarization fluctuations (FPF) of satellite HF to VHF beacon signals. The EPF are shown to be caused by the wave scattering from density irregularities, and it is shown that weak kilometer-scale density fluctuations are sufficient to cause the FPF of 20- to 54-MHz signals at locations not near the magnetic equator. The theory of single scattering is used to describe the FPF even in cases involving large density fluctuations, such as those of 41-MHz signals near the magnetic equator, and those of 136-MHz signals near the equatorial anomaly region.

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