2010
DOI: 10.1016/j.asr.2010.06.006
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An analysis of the topside ionosphere parameters based on the long-duration Irkutsk incoherent scatter radar measurements

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Cited by 3 publications
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“…According to the theory of incoherent scattering first presented by Gordon in 1958 [Gordon, 1958], ISR is the only equipment which has such ability. The measured area can be covered from 60 to 2000 km, and ISR has become the most powerful groundbased tool currently for the study of ionospheric structures and kinetic processes [Liu et al, 2007;Mathews, 1984], which makes it possible to study more ionosphere phenomena [Ratovsky et al, 2010]. Incoherent scatter radars use weak signals scattered by thermal fluctuations of upper atmospheric electrons [Evans, 1969;Dougherty and Farley, 1960;Brekke et al, 1974] to detect physical parameters of the ionosphere.…”
Section: Introductionmentioning
confidence: 99%
“…According to the theory of incoherent scattering first presented by Gordon in 1958 [Gordon, 1958], ISR is the only equipment which has such ability. The measured area can be covered from 60 to 2000 km, and ISR has become the most powerful groundbased tool currently for the study of ionospheric structures and kinetic processes [Liu et al, 2007;Mathews, 1984], which makes it possible to study more ionosphere phenomena [Ratovsky et al, 2010]. Incoherent scatter radars use weak signals scattered by thermal fluctuations of upper atmospheric electrons [Evans, 1969;Dougherty and Farley, 1960;Brekke et al, 1974] to detect physical parameters of the ionosphere.…”
Section: Introductionmentioning
confidence: 99%