2008
DOI: 10.1109/tps.2007.914189
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Modeling of Interaction of Acoustic Waves With Ionosphere

Abstract: We report on the results of experimental investigations of plasma discharges in air during which red Flashes similar to those arising in the upper layers of atmosphere have been observed. In addition, it was shown that under the influence of acoustic waves in the atmosphere, a response in the form of visible radiation was brought about, and pulsed electromagnetic waves were generated.

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Cited by 7 publications
(4 citation statements)
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“…We propose a new hydrodynamic analyticalnumerical model which includes the two-stage (consequent) transformation of SWs: (1) parametric transformations of two SW packets with frequencies ∼ 600 Hz and a modulation frequency ∼ 0.01 Hz to ISWs with the carrier difference frequency in the ELF range ∼ (10-100) Hz over a range of altitudes (0-0.5) km, and (2) the transformation of ISWs in the ELF range with the carrier frequency ∼ (10-100) Hz to AGWs in the ULF range with a frequency ∼ 0.01 Hz. This model is based on the parameters of the experiments with the PSG and corresponds to the experimental results qualitatively well (Parrot et al, 2007;Koshovyy, 1999;Kotsarenko et al, 1999;Soroka et al, 2006;Aramyan et al, 2008). We then discuss the physical consequences of these processes and the possibilities of their observations using satellites and ground-based instruments.…”
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confidence: 54%
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“…We propose a new hydrodynamic analyticalnumerical model which includes the two-stage (consequent) transformation of SWs: (1) parametric transformations of two SW packets with frequencies ∼ 600 Hz and a modulation frequency ∼ 0.01 Hz to ISWs with the carrier difference frequency in the ELF range ∼ (10-100) Hz over a range of altitudes (0-0.5) km, and (2) the transformation of ISWs in the ELF range with the carrier frequency ∼ (10-100) Hz to AGWs in the ULF range with a frequency ∼ 0.01 Hz. This model is based on the parameters of the experiments with the PSG and corresponds to the experimental results qualitatively well (Parrot et al, 2007;Koshovyy, 1999;Kotsarenko et al, 1999;Soroka et al, 2006;Aramyan et al, 2008). We then discuss the physical consequences of these processes and the possibilities of their observations using satellites and ground-based instruments.…”
mentioning
confidence: 54%
“…The maximum experimental value of the amplitude of the input velocity is v 0 = 420 m s −1 for our setup (Aramyan et al, 2008). The initial width of the SW beam is ρ 01 = (1-10) m in the horizontal plane.…”
Section: The First Frequency Transformmentioning
confidence: 89%
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