2006
DOI: 10.21236/ada509431
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An Atmospheric Turbulence Profile Model for Use in Army Wargaming Applications I

Abstract: Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing the burden, to Department of Defense, Washington Headquarters Services, Directorate for Informat… Show more

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Cited by 21 publications
(16 citation statements)
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“…The parameters v and A depend on the atmospheric conditions. For this paper we used the values A = 1.7 × 10 −14 m − 2 3 and v = 21 m/s, which are typical values at sea level during nighttime [70]. Once we have the waist of The variables follow those used in the text: S t is the transmitter's surface, S r is the receiver's surface, σ is the pointing error, d is the distance from the satellite to the ground station, and ζ is the elevation angle from ground.…”
Section: A Numerically Modelling Realistic Lossmentioning
confidence: 99%
“…The parameters v and A depend on the atmospheric conditions. For this paper we used the values A = 1.7 × 10 −14 m − 2 3 and v = 21 m/s, which are typical values at sea level during nighttime [70]. Once we have the waist of The variables follow those used in the text: S t is the transmitter's surface, S r is the receiver's surface, σ is the pointing error, d is the distance from the satellite to the ground station, and ζ is the elevation angle from ground.…”
Section: A Numerically Modelling Realistic Lossmentioning
confidence: 99%
“…with ζ the elevation angle of the satellite from the ground, h the altitude of the receiver, and C 2 n (z) the refractive-index structure constant, given by The parameters v and A depend on the atmospheric conditions. For this paper we used the values A = 1.7 × 10 −14 m − 2 3 and v = 21 m s −1 , which are typical values at sea level during nighttime [70]. Once we have the waist of the Gaussian distribution we can use a twodimensional convolution with the intensity profile I 2 ( v) that includes pointing error to obtain the overall beam profile I 3 ( v).…”
Section: Resultsmentioning
confidence: 99%
“…These values are often assumed by astronomers for nighttime conditions. However, the Hufnagel-Valley model is often not suitable for daytime conditions [12].…”
Section: Theoretical Backgroundmentioning
confidence: 99%