2021
DOI: 10.3390/atmos12121608
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A Survey of Structure of Atmospheric Turbulence in Atmosphere and Related Turbulent Effects

Abstract: The Earth’s atmosphere is the living environment in which we live and cannot escape. Atmospheric turbulence is a typical random inhomogeneous medium, which causes random fluctuations of both the amplitude and phase of optical wave propagating through it. Currently, it is widely accepted that there exists two kinds of turbulence in the aerosphere: one is Kolmogorov turbulence, and the other is non-Kolmogorov turbulence, which have been confirmed by both increasing experimental evidence and theoretical investiga… Show more

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Cited by 7 publications
(5 citation statements)
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“…By measuring and analyzing this constant, the turbulent variation characteristics of different geographical environments can be understood, which is beneficial in objectively assessing the impact of the atmosphere on FSO. 19 Currently, the Davis' inequality is the commonly used method to distinguish turbulence intensity according to C 2 n . In this study, we used this method to divide the urban atmospheric turbulence intensity during the observation period; its specific expression is 20…”
Section: Scintillation Methods Andmentioning
confidence: 99%
See 1 more Smart Citation
“…By measuring and analyzing this constant, the turbulent variation characteristics of different geographical environments can be understood, which is beneficial in objectively assessing the impact of the atmosphere on FSO. 19 Currently, the Davis' inequality is the commonly used method to distinguish turbulence intensity according to C 2 n . In this study, we used this method to divide the urban atmospheric turbulence intensity during the observation period; its specific expression is 20…”
Section: Scintillation Methods Andmentioning
confidence: 99%
“…Cn2 plays a crucial role in the study of light propagation and is one of the basic parameters in atmospheric optics. By measuring and analyzing this constant, the turbulent variation characteristics of different geographical environments can be understood, which is beneficial in objectively assessing the impact of the atmosphere on FSO 19 …”
Section: Scintillation Effect Analysismentioning
confidence: 99%
“…Eqs ( 3), (4), and (5) represent the mathematical expressions for the turbulence in each layer, with varying turbulence parameters and wave numbers [36][37][38]. where: z is a propagation distance that varies between z = 0 and z = L, is Kolmogorov turbulent index of refraction structure parameter in the boundary layer(has unit of m -2/3 ), is the non-Kolmogorov turbulent index of refraction structure parameter in the free troposphere (has unit of m -1/3 ), and is the non-Kolmogorov turbulent index of refraction structure parameter in the stratosphere(of m -2 units).…”
Section: Von Karman Atmospheric Turbulence Modelmentioning
confidence: 99%
“…The large eddies are broken into small eddies by transferring kinetic energy, and the small eddies continue to broken until the kinetic energy of the fluid is completely converted into internal energy. Kolmogorov 25 supplemented the statistical description. The model defined the outer and inner scale of turbulence 0 L and 0 l , in their ranges (inertial subrange), the eddies are considered to coexist and turbulence can achieve dynamic equilibrium.…”
Section: Turbulencementioning
confidence: 99%