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Whistler Waves' Propagation in Plasmas With Systems of Small‐Scale Density Irregularities: Numerical Simulations and Theory
Author(s) -
Zudin I. Yu.,
Zaboronkova T. M.,
Gushchin M. E.,
Aidaki. A.,
Korobkov S. V.,
Krafft C.
Publication year - 2019
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2019ja026637
Subject(s) - whistler , atmospheric duct , computational physics , physics , ionosphere , transverse plane , electron density , wave propagation , magnetic field , transmitter , plasma , radio wave , electromagnetic radiation , geophysics , optics , meteorology , telecommunications , quantum mechanics , channel (broadcasting) , structural engineering , atmosphere (unit) , computer science , engineering
The propagation of whistler waves in a magnetized plasma containing multiple small‐scale (100 m to 1 km) field‐aligned irregularities of enhanced electron density is considered analytically and by means of numerical simulations. Such systems of irregularities can develop in the upper ionosphere during the generation of density ducts by high‐frequency heating facilities and other types of active experiments. The simulation parameters are close to those of an active experiment where a whistler wave of 18 kHz emitted by a ground‐based very low frequency (VLF) transmitter was received onboard the DEMETER satellite at 700 km above the SURA heater. The study reveals a number of remarkable properties of the VLF waves' propagation, including the existence of specific waveguide modes of the small‐scale density structures and of a characteristic transverse size d 0 of the irregularities. Irregularities with small density enhancements around 10–20% and transverse sizes larger than d 0 ∼1 km can serve as separate waveguides for VLF waves. In their turn, single irregularities narrower than d 0 cannot be considered as individual ducting structures. Numerical simulations show that, for the analysis of the electromagnetic whistlers' propagation, a system of closely spaced irregularities with scales narrower than d 0 can be modeled by an equivalent ducting structure with a smoothed density profile. Such equivalent structure has the same ducting properties for whistlers and can be produced by averaging with a sliding window of a scale about d 0 the original density distribution.