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Plasma Theory of Solar Radar Echoes after Thirty Years

Published online by Cambridge University Press:  30 March 2016

Valentin Mel’nik*
Affiliation:
Institute of Radio Astronomy of National Academy of Sciences, 4 Chervonopraporna str., 310002, Kharkiv, Ukraine

Extract

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In 1967 Gordon made the revolutionary assumption that reflection of radar signal from the Sun can be explained by its scattering on microturbulence (Gordon 1973). In his first model it was ion-sound turbulence. Later he considered radar scattering on Langmuir turbulence. The principal opportunity to explain frequency displacements of radar echoes observed in James’ experiments (James 1966, 1970) was shown. However, it turned out (Gerasimova 1979) that the mechanism needed an impermissible high level of isotropic turbulence for the reflection with cross-sections σ = 10πR2ʘ.

Type
II. Joint Discussions
Copyright
Copyright © Astronomical Society of Pacific 2002

References

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Mel’nik, V.N. 1998, Radiofizika i Radioastronomiia, 3, 12; ibid., 3, 22 Google Scholar
Mel’nik, V.N. 1999, Solar Phys., 184, 363; Astronomy Letters, 25, 336 CrossRefGoogle Scholar