2015
DOI: 10.1201/b18922
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Acoustics in Moving Inhomogeneous Media

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Cited by 144 publications
(202 citation statements)
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“…The method uses the effective speed of sound approach wherein the moving atmosphere is replaced by a hypothetical motionless medium with an effective sound speed c eff ¼ c þ v x , where v x is the wind velocity component along the direction of propagation between the source and receiver. 42 In this study, the speed of sound is kept constant [c(x, z) ¼ 340 m/s] in the whole domain, and the propagation phenomena (i.e., refraction, diffraction, scattering) is solely due to the wind speed and its fluctuations around the wind turbine. This approach is representative of a neutrally stratified atmosphere on a day with high wind or thick cloud layers.…”
Section: Sound Propagation Modelmentioning
confidence: 99%
“…The method uses the effective speed of sound approach wherein the moving atmosphere is replaced by a hypothetical motionless medium with an effective sound speed c eff ¼ c þ v x , where v x is the wind velocity component along the direction of propagation between the source and receiver. 42 In this study, the speed of sound is kept constant [c(x, z) ¼ 340 m/s] in the whole domain, and the propagation phenomena (i.e., refraction, diffraction, scattering) is solely due to the wind speed and its fluctuations around the wind turbine. This approach is representative of a neutrally stratified atmosphere on a day with high wind or thick cloud layers.…”
Section: Sound Propagation Modelmentioning
confidence: 99%
“…The smaller value corresponds to the range of values reported in Ref. [15] near (flat) ground during a summer's day. Note that modelling temperature related turbulence is not fully consistent with the previously made assumption of a purely logarithmic wind speed profile; however, the main goal here is studying the effect of a scattering atmosphere.…”
Section: Turbulencementioning
confidence: 99%
“…The Kolmogorov turbulence spectrum can be considered as a universally applicable and realistic representation of the atmosphere in the inertial subrange [15]. Eight length scales are considered, ranging from 1.5 cm to 2 m, fitting in between the grid resolution and the extent of the simulation domain.…”
Section: Turbulencementioning
confidence: 99%
“…The appropriateness of the log-normal distribution to weak scattering is discussed in many texts on wave propagation in random media (Flatté et al 1979, Rytov et al 1989, Andrews and Phillips 2005, Ostashev and Wilson 2015. It follows from the Rytov approximation for the log-amplitude and the assumption that received signal consists of many independent additive contributions.…”
Section: B Log-normal (Weak Scattering In the Rytov Approximation)mentioning
confidence: 99%