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Generalized coherence functions for propagation in a random medium

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Abstract and Figures

We have derived the two-source, two-frequency mutual coherence functions for a spherical wave propagating in a random medium for the case when the receivers do not necessarily lie in the same transverse plane.
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1326 J. Opt. Soc. Am. A/Vol. 3, No. 8/August 1986
Generalized coherence functions for propagation in a
random medium
Ronald L. Fante
Avco Systems/Textron, Wilmington, Massachusetts 01887
Received October 26, 1985; accepted April 9, 1986
We have derived the two-source, two-frequency mutual coherence functions for a spherical wave propagating in a
random medium for the case when the receivers do not necessarily lie in the same transverse plane.
It is now well known",2that the electric field produced by a
planar source located in a weakly fluctuating random medi-
um can be calculated by employing the extended Huygens-
Fresnel principle. That is, for a medium in which the fluc-
tuations in the index of refraction are small in comparison
with the mean index and in which the spatial size of all
random inhomogeneities is large in comparison with a wave-
length, the electric field at a point (xo, yo, z) due to a source
field E(xl, y, 0) is given by (see Fig. 1)
E(po, zo; k) = Pi E(pl, 0)
X exp [i
2z (Po -p) 2+ .(po, Z0, P10; k)
(1)
where it is assumed that zo2
>> (p -p) 2.Also, po -- (xo, yo),
P1 (xi, Yl), k = 2r/X is the wavelength, and A
-- X(Po,
zo, p1,
0;
k) + iS(po, zo, p, 0;
k) is the additional complex phase (due to
the random medium) of a spherical wave propagating from
(p1,
0) to (po, z). It can be shown that 3
I dz' II d2p' nl(x', y',
27r do .z (z -Z')
r oik
( -p,)2(p
-p) 2(Po
-p) 211
X exp. ~
I+ / (2)
2 [z - z' Z/ J
where n(x', y', z') is the fluctuation in the index of refrac-
tion. It is found that Eq. (2) is valid, provided that (x 2) << 1,
where ( ) denotes an ensemble average. In this same do-
main of validity, x and S are Gaussian random variables.
The generalized mutual coherence function
(E(po z, k)E*(p/o, z'O, k'))
and other moments of the field can be computed by using
Eq. (1) along
with the fact that x and S are Gaussian random
variables. Consequently, all moments can be expressed in
terms of (xx'), (SS'), (xS'), and (x'S), where (xx') (x(po,
zo,
p, 0; k)x(p'o, z'o, p'l, 0, k')), etc. and the points (po,
z),
(p'o, z'o), etc. are shown in Fig. 1.
The purpose of this paper is to present the results for the
generalized two-source, two-frequency spherical-wave co-
herence functions (xx'), (SS'), etc. By employing Eq. (2)
and paralleling previous4analyses, it is readily shown (the
details are very lengthy and will be omitted) that, provided
that (x 2) << 1, kzo >>
1, k'zo >> 1, klo >>
1, and k'0>>
1, where
lo is the smallest size (often called the inner scale) of the
random inhomogeneities, the desired coherence functions
are
(XX') ' 22kk' Idv KdK4(I, )J0(Ka)
(5'{j L L(
X K2V 1/ 1/ V\
yOS
-[-1 ---- u
2
k' ZI k~ zO
FCSK20
[
V 1_V)+( V )]
{(SX')} 2 JZ°
{(SW) =7 Zrkk' fo
dv fo KdK'P(, 0)JO(Ka)
X in- -1- -11-- i
{ 2 k'( Z'oJ k ( Zo!]
-- snK2
V
[ 1-V ) 1_V )
+ sin
where it has been assumed that z'o 2 z. Also,
a Z0
--)+Pi P
(3)
(4)
(5)
J(.. .) is the zero-order Bessel function, and (K, 0) = (K,
Ky,
0), where (Kx,, Ky, K) is the wave-number spectrum of the
index-of-refraction fluctuations. The structure functions,
DXX
= ((X -x')2), etc., can be obtained directly from Eqs.
(3) and (4).
For Kolmogorov turbulence
VW ) 0.033Cn 2(v)exp(-K 2/Km2)
[, 2+ L -2]11/6
where Lo is the outer scale size of the random inhomogenei-
ties, C2is the index-of-refraction structure constant, and Km
is related to the inner scale lo as Km = 5 9 1/1o. When c is
0740-3232/86/081326-02$02.00 © 1986 Optical Society of America
Ronald L. Fante
WI
Chapter
This chapter deals with the propagation behavior of infinitely extensive plane light waves after passing through, and being scattered by, a (hypothetical) thin inhomogeneous atmospheric layer. The propagation behavior is examined in the near-field Fresnel space beyond the layer which, at this preliminary stage, we consider homogeneous free space. The behavior of the crucially important two-point two-wavelength correlation function of the complex amplitudes is examined as the waves propagate beyond the layer. The insights and results obtained in this chapter provide a foundation for the analysis given in the next chapter, which deals with wave propagation over extended atmospheric paths. When the two wavelengths coalesce, the function degenerates into the atmospheric MTF. For any atmospheric path, the latter function determines the resolution that can be obtained when observing over that path. The development of scintillation is examined in the space below the layer, the extent to which it occurs depends crucially on the size of the turbulence structures in the layer.
Book
This book lays out a new, general theory of light propagation and imaging through Earth's turbulent atmosphere. Current theory is based on the - now widely doubted - assumption of Kolmogorov turbulence. The new theory is based on a generalized atmosphere, the turbulence characteristics of which can be established, as needed, from readily measurable properties of point-object, or star, images. The pessimistic resolution predictions of Kolmogorov theory led to lax optical tolerance prescriptions for large ground-based astronomical telescopes which were widely adhered to in the 1970s and 1980s. Around 1990, however, it became clear that much better resolution was actually possible, and Kolmogorov tolerance prescriptions were promptly abandoned. Most large telescopes built before 1990 have had their optics upgraded (e.g., the UKIRT instrument) and now achieve, without adaptive optics (AO), almost an order of magnitude better resolution than before. As well as providing a more comprehensive and precise understanding of imaging through the atmosphere with large telescopes (both with and without AO), the new general theory also finds applications in the areas of laser communications and high-energy laser beam propagation. © Springer International Publishing Switzerland 2016. All rights reserved.
Chapter
This chapter deals with the propagation behavior of infinitely extensive plane light waves after passing through, and being scattered by a (hypothetical) thin inhomogeneous atmospheric layer. The propagation behavior is examined in the near-field Fresnel space beyond the layer which, at this preliminary stage, we consider homogeneous free space. The behavior of the crucially important, two-point two-wavelength correlation function of the complex amplitudes, S(x,y,x,y,λ,λ)S(x^{'} , y^{'} , x , y ,\lambda^{'} , \lambda ), is examined as the waves propagate beyond the layer. The insights and results obtained in this chapter provide a foundation for the analysis given in the next chapter, which deals with wave propagation over extended atmospheric paths. When the two wavelengths coalesce, function 0S(x,y,x,y,λ,λ)S(x^{'} , y^{'} , x , y ,\lambda^{'} , \lambda ) degenerates into the atmospheric MTF, S(x,y,x,y,λ)S(x^{'} , y^{'} , x , y , \lambda ). For any atmospheric path, the latter function determines the resolution that can be obtained when observing over that path. The development of scintillation is examined in the space below the layer; the extent to which it occurs depends crucially on the size of the turbulence structures in the layer.
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The first part of this paper is devoted to extending the Huygens-Fresnel principle to a medium that exhibits a spatial (but not temporal) variation in index of refraction. Utilizing a reciprocity theorem for a monochromatic disturbance in a weakly inhomogeneous medium, it is shown that the secondary wavefront will be determined by the envelope of spherical wavelets from the primary wavefront, as in the vacuum problem, but that each wavelet is now determined by the propagation of a spherical wave in the refractive medium. In the second part, the above development is applied to the case in which the index of refraction is a random variable; a further application of the reciprocity theorem results in a formula for the mean intensity distribution from a finite aperture in terms of the complex disturbance in the aperture and the modulation transfer function (MTF) for a spherical wave in the medium. The results are applicable for an arbitrary complex disturbance in the transmitting aperture in both the Fresnel and Fraunhofer regions of the aperture. Using a Kolmogorov spectrum for the index of refraction fluctuations and a second-order expression for the MTF, the formula is used to calculate the mean intensity distribution for a plane wave diffracting from a circular aperture and to give approximate expressions for the beam spreading at various ranges.
Chapter
Consideration is given to the properties of electromagnetic wave propagation in a random medium having large spatial inhomogeneities in comparison with the wavelength of the radiation. The magnitude of the fluctuations in the refractive index of the medium is assumed to be near unity. A generalized version of the Huygen-Fresnel principle is derived from the vector form of the Maxwell wave equation. Specific solutions are obtained for the second moment of the electric field in the medium, the effect of scintillations, and the interaction of radiation with a rough surface immersed in a random medium. The effect of random fluctuations in temperature, humidity, and pressure on the propagation of electromagnetic waves in the atmosphere is analyzed on the basis of the theoretical results.
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General formulations for temporal frequency spectra of the fluctuations of plane, spherical, and beam waves operating at two frequencies are given based on weak turbulence and frozen-in assumptions. The cross spectra and the coherence are obtained for the amplitude at two frequencies, the phase at two frequencies, and the amplitude at one frequency and the phase at another frequency. The results are examined in detail for plane and spherical waves. For the spectrum of the index of refraction kappa^{-n} in the inertial subrange, the amplitude spectrum behaves as k^{(5-n)/2} for omega rightarrow 0 and k^{2}omega^{1-n} for omega rightarrow infty . The phase spectrum for omegarightarrow 0 and for omegarightarrowinfty behaves as k^{2}omega^{1-n} with different constants. These results agree well with the experimental work of Janes et al. [11] at 9.6 and 34.5 GHz, and explains the ratio of the spectra at two frequencies. Also noted is the experimental slope of -2.6 as and for omega rightarrow infty which may be compared with 1-n = -2.66 using the Kolmogorov spectrum of n = 11/3 . The amplitude and phase coherence are calculated, and the results agree well with the experimental data. This agreement is indicative of the general validity of the theory for frequencies as low as 10sim30 GHz and the path length as long as 60 km. It is also shown that using the preceding theory, the wind velocity and the structure constant C_{n} can be deduced from the experimental data. Theoretical wind velocity of 15.6 knots obtained from the propagation data compares favorably with the meteorologically measured value of 14 knots, and two values of C_{n} obtained independently from the amplitude and phase measurements closely agree with each other.
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Effect of the Turbulent Atmosphere on Wave Propagation (National Technical Information Service, Springfield
  • V Tatarskii
V. Tatarskii, Effect of the Turbulent Atmosphere on Wave Propagation (National Technical Information Service, Springfield, Va., 1971).