The main ionospheric trough as a spatial boundary of VLF noise storms

Details The main ionospheric trough as a spatial boundary of VLF noise storms The main ionospheric trough as a spatial boundary of VLF noise storms

Dec 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990ge%26ae..30..911k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 30, Nov.-Dec. 1990, p. 911-914. In Russian.

Physics

1

Auroras, Earth Ionosphere, Ionospheric Disturbances, Magnetic Disturbances, Noise Storms, Very Low Frequencies, Diurnal Variations, Earth Surface, F Region, Ionization, Plasmasphere

Scientific paper

An abrupt termination of VLF noise emissions is observed at auroral and subauroral latitudes during magnetically disturbed periods at afternoon hours. Temporally, this termination coincides with an anomalous ionization drop in the F-region (i.e., the passage of the main ionospheric trough above the observation point). Thus, on the earth's surface in the afternoon sector the ionospheric trough is a spatial boundary for the recording of plasmaspheric VLF noise storms on the earth's surface.

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