Subauroral VLF-ELF emissions and the main ionospheric trough

Details Subauroral VLF-ELF emissions and the main ionospheric trough Subauroral VLF-ELF emissions and the main ionospheric trough

Apr 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ge%26ae..25..266k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 25, Mar.-Apr. 1985, p. 266-271. In Russian.

Mathematics

Probability

Emission Spectra, Ionospheric Disturbances, Plasmapause, Troughs, Vlf Emission Recorders, Auroral Zones, High Energy Electrons, Magnetospheric Instability, Very Low Frequencies, Whistlers

Scientific paper

VLF observations at the Sogra-Kerguelen conjugate points are examined. It is shown that the probability of the occurrence of chorus and hiss bursts on the earth surface is associated with the location of the projection of the plasmapause and the main ionospheric trough (MIT). The MIT is found to play a large role in channeling VLF waves from the magnetosphere to the earth surface. The channeling of choruses is effected by the polar edge of the trough, while the channeling of ELF hiss is effected (in quiet and moderately disturbed periods) by the equatorial edge. During intense magnetic disturbances, hiss can be channeled toward the earth by both edges of the MIT.

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