IEE Colloquium on Remote Sensing of the Propagation Environment 1996
DOI: 10.1049/ic:19961186
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Use of radiosonde data in propagation prediction

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Cited by 5 publications
(9 citation statements)
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“…less negative) than usual, or even positive, sub-refraction occurs, where the ray bends less than usual towards the earth, even bending upwards in the case of a positive gradient and the range reduces. Sub-refraction occurs when warm moist air flows over a cool ocean surface or over a cooler air mass just above the ocean surface [2,17].…”
Section: A Refractivity Gradient In the Lowest Atmosphericmentioning
confidence: 99%
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“…less negative) than usual, or even positive, sub-refraction occurs, where the ray bends less than usual towards the earth, even bending upwards in the case of a positive gradient and the range reduces. Sub-refraction occurs when warm moist air flows over a cool ocean surface or over a cooler air mass just above the ocean surface [2,17].…”
Section: A Refractivity Gradient In the Lowest Atmosphericmentioning
confidence: 99%
“…β 0 represents the percentage of time in which the value of ΔN is less than or equal to -100 N/km [1,2,5]. It is derived from ΔN statistics in the lowest 100 m of the atmosphere.…”
Section: B β 0 Statisticsmentioning
confidence: 99%
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“…The k-factor can be calculated from the rate of change of the refractive index with height and the actual Earth's radius, a, using Snell's law in spherical geometry, knowing that N = (n-1) × 10 6 , where a is given by unit of nmi (a = 6371 km = 3440 nmi). The k-factor value must be multiplied by the actual Earth's radius, a, in order to plot the propagation paths as straight lines [1,3].…”
Section: Important Propagation Parametersmentioning
confidence: 99%
“…Some linear and exponential models [2,4,5] have been proposed to estimate the vertical profile from existing N s data. Several studies on refractivity analysis have been carried out for temperate climates all over the world [6][7][8][9][10][11], while a few are available for the unique subtropical climate of the Arabian Gulf region [12][13][14][15][16][17]. Three important atmospheric layers, namely 65 m, 100 m and 1 km layers above the ground are analyzed and the relevant propagation parameters are derived for the design of terrestrial communication systems operating in such climate.…”
Section: Introductionmentioning
confidence: 99%