
generally in the context of wave propagation in random media with long-range correlations that we describe
below. In this paper we write Φas
Φ(x, |ˆp−ˆ
k|) := a(|ˆp−ˆ
k|)
|ˆp−ˆ
k|2+α(x)=1
21+α(x)/2ρ(x, ˆ
k·ˆp),with ρ(x, s) := ap2(1 −s)
(1 −s)1+α(x)/2s∈[−1,1).(4)
Above, α:R3−→ [0,2) accounts for the slow variations of scattering across the ambient space, and ais a smooth
bounded function characterizing some statistical properties of the medium and such that a(0) >0. Practical
examples are given further. A direct calculation shows that (3) holds when α∈[0,2). Also, the integral in (2)
has to be understood in the principal value sense when α∈[1,2), see [23]. The multifractional terminology
that we use is motivated by the fact that the unbounded operator Qcan be expressed as a (multi)-fractional
Laplace-Beltrami operator (−∆S2)α(x)/2on the unit sphere up to a bounded operator w.r.t. the ˆ
kvariable
[22, 23].
We would like to emphasize that we focus in this work on kernels of the form (4) for simplicity of the
exposition, and that our method applies, after proper decomposition (see [23]), to more general kernels that
behave like (4) at the singularity.
The RTE can be derived from high frequency wave propagation in random media, see e.g. [49]. In such a
context, the velocity field c(x)has the form
1
c2(x)=1
c2
01 + √η V0x, x
η x∈R3, η ≪1,
where c0is the background velocity (that we set to one in the sequel for simplicity), V0is a mean zero random
field modeling fluctuations around the background, and ηis the correlation length of the random medium,
assumed to be small after proper rescaling. The first variable in V0represents the slow variations of the random
perturbations, while the second one corresponds to their high frequency oscillations. The latter are responsible
for the strong interaction between the wave and the medium over sufficient distances. The scattering kernel Φ
is related to the correlation function of V0, and assuming V0is stationary (in the statistical sense) with respect
to the fast variable, a kernel of the form (4) can be obtained from random fields such that
E[V0(x, x′)V0(y, y′)] = pλ(x)λ(y)ZR3
a(|p|)
|p|1+ α(x)+α(y)
2
eip·(x′−y′)dp, (5)
with αranging from 0to 2. Denoting by R(x)the expectation in (5) with y=x,y′=x′+x/η, one can
show that Rbehaves like |x|α(x)−2for |x| ≫ 1, and is therefore not integrable. This is how random fields
with long-range correlations are defined, as opposed to random fields with short-range correlations that exhibit
an integrable correlation function. This approach is of practical interest in biomedical imaging as media with
long-range correlations are able to reproduce experimentally observed power-law attenuations associated with
effective fractional wave equations [20, 25]. The value of the exponents is related to the rate of decay of the
correlation function R, and depends on the nature of the imaged tissues as reported in [14, 26, 27]. Variations
of this exponent can then be used for diagnosis purposes [38, 47].
In Figure 1, we provide examples of such 2D random fields. The top-left picture represents a random
medium with short-range correlations (with a standard Gaussian covariance kernel), while the top-right picture
illustrates a random medium with long-range correlations with α≡1. Because of the singularity at p= 0, one
can observe significantly larger statistical patterns than in the short-range case. In the bottom two pictures,
we highlight the roles of λand α:λcharacterizes scattering regions, and αdefines the correlation structure.
In the inner circle of the bottom-left picture we have α≡0.1, which tends to create shorter range fluctuations
than in the outside where α≡1. In the bottom-right picture, we have a three-layer model for αin which the
inner band exhibits smaller statistical patterns than the outer ones. This type of model is used for modeling
non-Kolmogorov atmospheric turbulences, while standard atmospheric turbulence is modeled with the so-called
Kolmogorov power spectrum
Φ(|k|)∝a(|k|)
|k|11/3,
for |k|in the inertial range of turbulence. This corresponds to the case α= 5/3. This case is not always valid
in experiments as reported in [4, 52, 55], and the statistics of atmospheric turbulence have been shown to vary
with altitude. Models have been derived for instance (see [35] for a review) by considering three ranges (0-2km,
2-8km, and above 8km) with distinct power laws (see Figure 16 for an illustration).
2