2015
DOI: 10.1049/el.2015.0195
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Modelling radio refractive index in the atmospheric surface layer

Abstract: Knowledge of the refractive index profile at radio frequencies in the surface layer of the atmosphere is required to predict the performance of terrestrial radio systems, and although a constant gradient of refractivity with height is often assumed, both measurements and theory suggest that gradients in the lowest 20 m of the atmosphere may often be greater than those above this level. For the special case of evaporation ducts over water in a neutral atmosphere, a logarithmic refractivity profile is normally a… Show more

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Cited by 8 publications
(3 citation statements)
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“…A common feature of these studies is the assumption that a linear positive refractivity gradient is the likely worst-case of a subrefractive atmosphere. Boundary layer similarity theory [17] indicates that surface refractivity gradients are likely to be stronger near the surface than at greater heights, and a subrefractive profile of this non-linear form has been shown to be capable of greater attenuation on a terrestrial path than a linear gradient with the same increase in refractivity over the lowest 100 m of the atmosphere [18].…”
Section: B Median Depression Fadingmentioning
confidence: 99%
“…A common feature of these studies is the assumption that a linear positive refractivity gradient is the likely worst-case of a subrefractive atmosphere. Boundary layer similarity theory [17] indicates that surface refractivity gradients are likely to be stronger near the surface than at greater heights, and a subrefractive profile of this non-linear form has been shown to be capable of greater attenuation on a terrestrial path than a linear gradient with the same increase in refractivity over the lowest 100 m of the atmosphere [18].…”
Section: B Median Depression Fadingmentioning
confidence: 99%
“…The dominant clear-air characteristics of the atmosphere affecting radio propagation are vertical moisture gradients and temperature gradients, as they produce vertical refractive index gradients, which cause the predominantly horizontally propagating radio signals to curve up or down. It is important to not only know the mean gradient over the surface layer; gradient variations within the surface layer may have a significant effect [22].…”
Section: Examples Of Gls With Regular and Irregularly Sampled Datamentioning
confidence: 99%
“…Simplified models based on a mass of historical detecting data have been studied extensively, for example, linear model, exponential model, double exponential model, Hopfield model, and subsection model [1][2][3]. A retrieval algorithm using ground-based global positioning system (GPS) is developed to establish the atmospheric refractivity profile model [4][5][6].…”
Section: Introductionmentioning
confidence: 99%