Ionospheric modification with a VLF transmitter

Details Ionospheric modification with a VLF transmitter Ionospheric modification with a VLF transmitter

Oct 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19.2071i&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 19, no. 20, p. 2071-2074.

Physics

13

D Region, Ionospheric Heating, Night Sky, Radio Transmitters, Very Low Frequencies, Ionospheric Electron Density, Three Dimensional Models

Scientific paper

Detectable heating of the nightime D region by a 28.5 kHz signal is observed in 16 out of 144 cases with events occurring under conditions of moderate to low D region electron densities as represented by the unperturbed VLF signal levels. Three dimensional modeling of the effects of NAU heating on a probe VLF signal predicts values in general agreement with observations and suggests that maximum effects should occur under tenuous D region conditions.

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