2017
DOI: 10.1007/s11141-017-9766-2
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On Features of the Generation of Artificial Ionospheric Irregularities with Transverse Scales of 50–200 m

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Cited by 2 publications
(3 citation statements)
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“…In the work of Bolotin et al. (2017), ionosonde signals were used for aspect scattering from irregularities of 50–200 m, and it was supposed that these irregularities appear most likely as the nonlinear cascade over the turbulence spectrum (Erukhimov et al., 1987).…”
Section: Results Of the Joint Sura‐norsat‐1 Experimentsmentioning
confidence: 99%
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“…In the work of Bolotin et al. (2017), ionosonde signals were used for aspect scattering from irregularities of 50–200 m, and it was supposed that these irregularities appear most likely as the nonlinear cascade over the turbulence spectrum (Erukhimov et al., 1987).…”
Section: Results Of the Joint Sura‐norsat‐1 Experimentsmentioning
confidence: 99%
“…The "magnetic zenith" effect and nonlinear plasma structuring as a result of self-focusing of the pump wave into plasma regions filled with small-scale artificial ionospheric irregularities elongated along the geomagnetic field leads to an increase in the generation of irregularities with scales from hundred meters to a kilometer (Frolov, 2017;Gurevich, 2007). In the work of Bolotin et al (2017), ionosonde signals were used for aspect scattering from irregularities of 50-200 m, and it was supposed that these irregularities appear most likely as the nonlinear cascade over the turbulence spectrum (Erukhimov et al, 1987).…”
Section: 1029/2020gl088462mentioning
confidence: 99%
“…We cannot but propose a mechanism for the interaction of a powerful radio wave with plasma, where under such ionospheric conditions, it would lead to the generation of intense artificial ionospheric irregularities. The observed phenomenon is connected with the presence of strong natural F spread (with strong natural irregularities with l ⊥ from 100 m to several kilometers) when the irregularities with l ⊥ ≈ 300–800 m are enhanced by powerful radio waves due to its self‐focusing instability, and at the second stage, these irregularities due to their nonlinear transformation give rise to irregularities with l ⊥ ≈ 100–200 m (Bolotin et al, 2017). In this case, strong scattering of radio waves in the ionosphere HF‐disturbed volume takes place as proposed by Zabotin et al (2002) together with F spread generation as it was observed in our experiments.…”
Section: Satellite Data Analysismentioning
confidence: 99%