Nonlinear hydrodynamic VLF wave scattering in the earth's magnetosphere

Details Nonlinear hydrodynamic VLF wave scattering in the earth's magnetosphere Nonlinear hydrodynamic VLF wave scattering in the earth's magnetosphere

Mar 1973

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1973p%26ss...21..359t&link_type=abstract

Planetary and Space Science, Volume 21, Issue 3, p. 359-366.

Physics

7

Scientific paper

The paper deals with a nonlinear instability of quasi-monochromatic VLF signals and whistlers in the Earth's magnetosphere due to induced scattering. The instability growth rates and the threshold values of the signal amplitude at which the instability occurs have been found. The instability is shown to be more effectively excited when the initial transverse VLF wave transforms into plasma oscillations at the lower hybrid resonance (LHR) frequency and may be responsible for the phenomena such as trigger LHR emission, the amplitude and phase modulation of artificial VLF signals and be the origin of some types of discrete VLF signals.

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