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Article

Probability Density Functions in Homogeneous and Isotropic Magneto-Hydrodynamic Turbulence

Laboratoire de Physique, Université de Lyon, ENS de Lyon, Université Claude Bernard Lyon 1, CNRS, F-69342 Lyon, France
Atmosphere 2020, 11(4), 382; https://doi.org/10.3390/atmos11040382
Submission received: 15 March 2020 / Revised: 6 April 2020 / Accepted: 8 April 2020 / Published: 14 April 2020

Abstract

:
We derive a hierarchy of evolution equations for multi-point probability density functions in magneto-hydrodynamic (MHD) turbulence. We discuss the relation to the moment hierarchy in MHD turbulence formulated by Chandrasekhar (S. Chandrasekhar, Proc. R. Soc. Lond. A 1951, 204, 435–449) and derive a functional equation for a joint characteristic functional, which can be considered as the analogon to the Hopf functional in hydrodynamic turbulence. Furthermore, we develop a closure method for the evolution equation of the single-point magnetic field probability density function, which is based on a joint Gaussian assumption for unclosed terms. It is explicitly shown that this closure, together with the assumptions of homogeneity and isotropy, leads to vanishing nonlinear terms. We discuss the implications of this finding for magnetic field generation and give a brief outlook on an axisymmetric theory, which includes a mean magnetic field.

1. Introduction

The investigation of magneto-hydrodynamic (MHD) turbulence by statistical methods has a longstanding tradition, which can be traced back to the works of Chandrasekhar [1] and Batchelor [2], as well as to the subdivision of mean field electrodynamics put forth by Steenbeck, Krause, and Rädler [3] (for further references, see [4,5]). Recent developments in statistical magnetohydrodynamics include an analytical treatment of weak MHD turbulence [6], a phenomenological description for the energy spectrum based on the dynamical alignment of velocity and magnetic field fluctuations [7,8], and the derivation of relations between longitudinal and transverse structure functions [9] similar to the ones of hydrodynamic turbulence [10,11,12]. On the other hand, improved measurements in the solar wind [13,14] along with an ever-growing number of experiments, which operate with liquid sodium under turbulent conditions in order to study the dynamo effect [15,16,17], are of great importance for the direct assessment of certain statistical quantities.
Therefore, a comprehensive statistical formulation of MHD turbulence will also lead to considerable advances in the modeling of these astrophysical and experimental MHD flows. Nonetheless, similar to the case of hydrodynamic turbulence, such a statistical description of MHD turbulence is complicated by the occurrence of anomalous statistics of velocity and magnetic field fluctuations at small scales, which is commonly referred to as intermittency [18]. To some degree, intermittency effects in fully developed MHD turbulence are even more pronounced than in ordinary turbulence, a fact that is commonly attributed to the geometrical structures observed in MHD turbulence, i.e., nearly singular current and vortex sheets [19,20]. Moreover, the Alfvén effect [21] introduces additional nonlocalities in the multi-point hierarchy of MHD flows, which will be discussed in more detail in Section 2. Therefore, due to pronounced deviations from Gaussianity and additional nonlocalities in the multi-point hierarchy of MHD turbulence, finding appropriate methods or assumptions to close the hierarchy at a certain stage [22,23] might prove to be even more difficult than in ordinary turbulence.
However, the presence of the magnetic field in conducting turbulent flows can also have a regularizing effect on the nonlinearities of the MHD equations. For instance, as shown by direct numerical simulations of MHD turbulence [9], the additional possibility for the velocity field to align with the magnetic field leads to depleted pressure contributions in regions with preferred alignment (anti-alignment).
In the following, we derive evolution equations for multi-point velocity and magnetic field probability density functions (PDFs) directly from the MHD equations. The emerging hierarchy can be considered as the counterpart to the hierarchy in hydrodynamic turbulence by Lundgren [24], Monin [25], and Novikov [26] (we also refer the reader to [27] for further reviews) and is similar to the BBGKY hierarchy of statistical mechanics. We will then proceed to discuss a possible closure method on the basis of a joint Gaussian assumption for velocity and magnetic field statistics.

2. Derivation of a Hierarchy of PDF Equations

The purpose of this section is to derive evolution equations for multi-point velocity and magnetic field PDFs in an analogous manner to the hydrodynamic case discussed in the seminal work by Lundgren [24]. To this end, we consider the MHD equations in the following form:
t u ( x , t ) + u ( x , t ) · x u ( x , t ) h ( x , t ) · x h ( x , t ) = x p ( x , t ) + ν x 2 u ( x , t ) ,
t h ( x , t ) + u ( x , t ) · x h ( x , t ) h ( x , t ) · x u ( x , t ) = λ x 2 h ( x , t ) ,
where ν denotes the kinematic viscosity, λ the magnetic diffusivity, and p ( x , t ) the total pressure, i.e., hydrodynamic and magnetic pressure. Furthermore, it should be stressed that in this particular form of the MHD equations, the magnetic field has the dimensions of a velocity. The MHD equations are completed by the incompressibility conditions · u ( x , t ) and · h ( x , t ) .
We define single-point magnetic and velocity field PDFs according to:
f u ( v , x , t ) = δ ( v u ( x , t ) ) ,
f h ( b , x , t ) = δ ( b h ( x , t ) ) ,
where the brackets denote ensemble averages over all possible realizations of the velocity field u ( x , t ) and magnetic field h ( x , t ) . In principle, the following treatment could also be carried out in terms of Elsässer fields z ± = u ± h . However, due to the different transformation behavior of h (axial vector) and u (polar vector) under reflexions, it will be more appropriate to work in the original fields, especially with regard to the tensor calculus of isotropic and homogeneous MHD turbulence [1,9,28] that will be used in Section 4. For later convenience, we also define the two-point PDFs:
f u u ( v , x ; v , x , t ) = δ ( v u ( x , t ) ) δ ( v u ( x , t ) ) ,
f u h ( v , x ; b , x , t ) = δ ( v u ( x , t ) ) δ ( b h ( x , t ) ) ,
f h h ( b , x ; b , x , t ) = δ ( b h ( x , t ) ) δ ( b h ( x , t ) ) .
The evolution equation for the single-point velocity field can be obtained by deriving the single-point velocity PDF (3) with respect to time:
t f u ( v , x , t ) = v · u ( x , t ) t δ ( v u ( x , t ) ) .
Here, we have to insert the temporal evolution of the velocity field, which is given by Equation (1), and treat the corresponding terms separately. The treatment is similar to the hydrodynamic case [24] and is discussed in Appendix A.1. The evolution equation for the single-point velocity PDF thus reads:
t + v · x f u ( v , x , t ) = v · d x δ ( x x ) d b b · x b f u h ( v , x ; b , x , t ) + 1 4 π v · d x x 1 | x x | d v v · x 2 f u u ( v , x ; v , x , t ) 1 4 π v · d x x 1 | x x | d b b · x 2 f u h ( v , x ; b , x , t ) ν v · d x δ ( x x ) x 2 d v v f u u ( v , x ; v , x , t ) ,
and therefore couples to the two-point PDFs (5) and (6). By the same token, we can derive the single-point magnetic field PDF (4) with respect to time:
t f h ( b , x , t ) = b · h ( x , t ) t δ ( b h ( x , t ) ) ,
insert the evolution Equation (2), and relate the corresponding terms to the two-point PDFs (6) and (7), which are discussed in Appendix A.2. The counterpart to the single-point velocity PDF Equation (9), i.e., the evolution equation for the single-point magnetic field PDF, thus reads:
t f h ( b , x , t ) + d v v · x f u h ( v , x ; b , x , t ) = b · d x δ ( x x ) d v b · x v f u h ( v , x ; b , x , t ) λ b · d x δ ( x x ) x 2 d b b f h h ( b , x ; b , x , t ) ,
which, again, is an unclosed equation since it couples to the two-point quantities (6) and (7). Equations (9) and (11) are the first equations in an infinite chain of evolution equations, e.g., the two-point PDFs (5)–(7) will couple to three-point PDFs, and so forth. Typical assumptions that are used in order to close such hierarchies include the assumption of statistical independence, as well as Gaussian assumptions [27] and will be further discussed in Section 3.2.
In comparison to ordinary turbulence where unclosed terms are due to nonlocal pressure contributions and the viscous term, the Alfvén effect introduces additional nonlocalities in the multi-point hierarchy. Indeed, it can readily be seen that both l.h.s. of Equations (9) and (11) are Galilei invariant, i.e., they are unchanged under the transformation v v + V , b b , and x x V t , whereas for v v and b b + B , B cannot be removed by a Galilei transformation due to the first terms on the r.h.s. of Equations (9) and (11). Obviously, the latter transformation behavior is inherited from the basic MHD Equations (1) and (2).
In order to generalize the results for the one-point magnetic and velocity field PDF to an arbitrary number of points, we define the ( n + m ) -point joint velocity-magnetic field PDF:
f n u , m h ( { v i , x i } ; { b j , y j } , t ) = i = 1 n j = 1 m δ ( v i u ( x i , t ) ) δ ( b j h ( y j , t ) ) .
A treatment similar to the one described in Appendix A yields the following evolution equation for the ( n + m ) -point joint velocity-magnetic field PDF:
t + i = 1 n v i · x i f n u , m h ( { v i , x i } , { b j , y j } , t ) + j = 1 m d v v · y j f ( n + 1 ) u , m h ( v , y j ; { v i , x i } ; { b j , y j } , t ) = i = 1 n v i · d x δ ( x i x ) d b b · x b f n u , ( m + 1 ) h ( { v i , x i } ; b , x ; { b j , y j } , t ) j = 1 m b j · d y δ ( y j y ) d v b j · y v f ( n + 1 ) u , m h ( v , y ; { v i , x i } ; { b j , y j } , t ) + 1 4 π i = 1 n v i · d x x i 1 | x i x | d v v · x 2 f ( n + 1 ) u , m h ( v , x ; { v i , x i } ; { b j , y j } , t ) 1 4 π i = 1 n v i · d y x i 1 | x i y | d b b · y 2 f n u , ( m + 1 ) h ( { v i , x i } ; b , y ; { b j , y j } , t ) ν i = 1 n v i · d x δ ( x i x ) x 2 d v v f ( n + 1 ) u , m h ( v , x ; { v i , x i } ; { b j , y j } , t ) λ j = 1 m b j · d y δ ( y j y ) y 2 d b b f n u , ( m + 1 ) h ( { v i , x i } ; b , y ; { b j , y j } , t ) .
Equation (13) is the most general evolution equation for multi-point PDFs in MHD turbulence. In the following section, we will discuss a more compact statistical description of MHD turbulence in terms of functional equations. Here, we briefly want to relate the PDF hierarchy Equation (13) to the moment hierarchy in MHD turbulence in the example of two-point correlation functions. To this end, we take the moments of the two-point PDFs (5)–(7), which result in the well-known two-point correlation functions of MHD turbulence:
C i j u u ( x ; x , t ) = d v v i d v v j f u u ( v , x ; v , x , t ) = u i ( x , t ) u j ( x , t ) ,
C i j u h ( x ; x , t ) = d v v i d b b j f u h ( v , x ; b , x , t ) = u i ( x , t ) h j ( x , t ) ,
C i j h h ( x ; x , t ) = d b b i d b b j f h h ( b , x ; b , x , t ) = h i ( x , t ) h j ( x , t ) ,
where the indices i and j now denote vector components. It can be shown (see Appendix B) that in taking the moments (14)–(16) of the evolution Equation (13) for (5)–(7), one indeed obtains equations relating moments of second order to moments of third order. This moment hierarchy can be considered as the MHD analogon to the Friedmann–Keller hierarchy [29] and was first derived by Chandrasekhar [1], who also addressed the implications of homogeneity and isotropy in an invariant theory of MHD turbulence. We will make use of this invariant theory in Section 4, which discusses a closure method for the single-point magnetic field PDF Equation (11).
We will end this section with some general comments on the multi-point PDF Equation (13). First, fusing different points of the velocity and the magnetic field y l x k in the evolution Equation (13) can be achieved by the integration:
f n u , m h ( v 1 , x 1 ; ; v k , x k ; ; v n , x n ; b 1 , y 1 ; ; b l , x k ; ; b m , y m , t ) = d y l δ ( y l x k ) f n u , m h ( { v i , x i } ; { b j , y j } , t ) .
This integration can be carried out directly for all terms in Equation (13) except for the third term for j = l of the l.h.s., which yields:
d y l δ ( y l x k ) d v v · y l f ( n + 1 ) u , m h ( v , y l ; { v i , x i } ; { b j , y j } , t ) = d y l ( y l δ ( y l x k ) ) x k δ ( y l x k ) · d v v f ( n + 1 ) u , m h ( v , y l ; { v i , x i } ; { b j , y j } , t ) = d v v · x k d y l δ ( y l x k ) f ( n + 1 ) u , m h ( v , y l ; { v i , x i } ; { b j , y j } , t ) = d v v · x k f ( n + 1 ) u , m h ( v , x k ; v 1 , x 1 ; ; v k , x k ; ; v n , x n ; b 1 , y 1 ; ; b l , x k , ; b m , y m , t ) δ ( v v k ) f n u , m h ( v 1 , x 1 ; ; v k , x k ; ; v n , x n ; b 1 , y 1 ; ; b l , x k ; ; b m , y m , t ) = v k · x k f n u , m h ( v 1 , x 1 ; ; v k , x k ; ; v n , x n ; b 1 , y 1 ; ; b l , x k ; ; b m , y m , t ) ,
where we made use of the so-called coincidence property of the multi-point PDF (12). Further points can be fused by the same procedure, which thus allows access to the evolution equations of mixed PDFs with a single point of reference as given, for instance, by Equation (6) for x = x . Latter statistical quantities are frequently encountered in spacecraft measurements, such as those in the solar wind by Ulysses, where oftentimes, Taylor’s hypothesis (with respect to the bulk wind speed in the laboratory frame) is invoked in order to characterize spatial fluctuations of velocity and magnetic fields with the same point of reference [30,31]. Moreover, bridging to velocity and magnetic field increment PDFs can be achieved by similar procedures to the ones described by Ulinich and Lyubimov for the case of hydrodynamic turbulence [32]. Similarly to the derivation of the correlation function hierarchy from the multi-point hierarchy (13) discussed in Appendix B, the latter multi-increment evolution equations can also be used in order to derive a hierarchy of structure functions in MHD turbulence [9].

3. Functional Formulation of MHD Turbulence

In the previous section, we derived a hierarchy of evolution equations for PDFs in MHD turbulence, which culminated in the generalized evolution equation for the ( n + m ) -point PDF Equation (13). Owing to the fact that the MHD Equations (1) and (2) form a classical field theory, a complete description of the Eulerian statistics is contained in the joint characteristic functional [33]:
ϕ [ α ( x ) , β ( x ) , t ] = e i d x α ( x ) · u ( x , t ) + β ( x ) · h ( x , t ) .
This functional can be used in order to project on both multi-point PDF Equation (12) and multi-point correlations such as Equations (14)–(16). In a more general way, the ordinary characteristic function:
φ ( { α i , x i } ; { β j , y j } , t ) = exp i i = 1 n α i · u ( x i , t ) exp i j = 1 m β j · h ( y j , t ) ,
coincides with the characteristic functional Equation (19) evaluated at discrete points of the real-valued fields α ( x ) and β ( x ) , namely for:
α ( x ) = i = 1 n α i δ ( x x i ) , and β ( x ) = j = 1 m β j δ ( x y j ) .
Accordingly, by Fourier transforming Equation (20), it can be seen that the ( n + m ) -point PDF Equation (12) is related to the joint characteristic functional by:
f n u , m h ( { v i , x i } ; { b j , y j } , t ) = i = 1 n d α i ( 2 π ) 3 j = 1 m d β i ( 2 π ) 3 e i i = 1 n α i · v i e i j = 1 m α j · b j ϕ i = 1 n α i δ ( x x i ) , j = 1 m β j δ ( x y j ) , t .
In the following section, we briefly derive an evolution equation for the joint characteristic functional (19), whereas Section 3.2 describes its Gaussian approximation.

3.1. Evolution Equation for the Characteristic Functional in MHD Turbulence

An evolution equation for the joint characteristic functional can be obtained by deriving Equation (19) with respect to time:
t ϕ [ α ( x ) , β ( x ) , t ] = i d x α ( x ) · u ( x , t ) t + β ( x ) · h ( x , t ) t e i d x α ( x ) · u ( x , t ) + β ( x ) · h ( x , t ) .
Inserting the MHD Equations (1) and () yields:
t ϕ [ α ( x ) , β ( x ) , t ] = d x α j ( x ) i x k δ 2 δ α k ( x ) δ α j ( x ) δ 2 δ β k ( x ) δ β j ( x ) + ν 2 x k x k δ δ α j ( x ) + x j d x 4 π | x x | 2 x k x l δ 2 δ α k ( x ) δ α l ( x ) δ 2 δ β k ( x ) δ β l ( x ) ϕ [ α ( x ) , β ( x ) , t ] + d x β j ( x ) i x k δ 2 δ α k ( x ) δ β j ( x ) δ 2 δ β k ( x ) δ α j ( x ) + λ 2 x k x k δ δ β j ( x ) ϕ [ α ( x ) , β ( x ) , t ] .
Due to the incompressibility condition for the velocity field, the joint characteristic functional is invariant under the transformation:
α j ( x ) = α ˜ j ( x ) + x j ψ ( x ) ,
and the pressure term in Equation (24) can be eliminated, which yields:
t ϕ [ α ( x ) , β ( x ) , t ] = d x α ˜ j ( x ) i x k δ 2 δ α k ( x ) δ α j ( x ) δ 2 δ β k ( x ) δ β j ( x ) + ν 2 x k x k δ δ α j ( x ) ϕ [ α ( x ) , β ( x ) , t ] + d x β j ( x ) i x k δ 2 δ α k ( x ) δ β j ( x ) δ 2 δ β k ( x ) δ α j ( x ) + λ 2 x k x k δ δ β j ( x ) ϕ [ α ( x ) , β ( x ) , t ] .
This linear functional equation for the joint characteristic functional can be considered as the most compact statistical description of MHD turbulence and is the analog of Hopf’s functional formulation of hydrodynamic turbulence [19,33,34]. Therefore, like in turbulent flows, the statistical dynamics of MHD turbulence is a linear problem, whereas individual realizations are governed by nonlinear partial differential equations. Moreover, the linearity of Equation (24) necessarily implies that the joint characteristic functional (19) obeys the superposition principle: if the characteristic functionals ϕ ( i ) [ α ( x ) , β ( x ) , t ] are solutions of Equation (24) subject to the corresponding initial conditions ϕ ( i ) [ α ( x ) , β ( x ) , t = 0 ] , then ϕ ( i ) [ α ( x ) , β ( x ) , t ] is a linear combination of these solutions.

3.2. Cumulant Expansion and the Implications of Vanishing Higher Order Cumulants

In the following, we consider the implications of the vanishing of cumulants higher than second order. Evidently, in the latter case, the velocity and magnetic field are distributed according to a joint normal distribution. In fully developed MHD turbulence, however, such a scenario is quite unrealistic, and empirical findings suggest strongly non-Gaussian behavior at small scales, which is oftentimes attributed to the occurrence of nearly singular current and vortex sheets [9,35]. Nonetheless, as described in the next sections, we are solely interested in using the joint Gaussian approximation for mixed velocity and magnetic field conditional two-point moments in the single-point magnetic field evolution Equation (4). Hence, as described in Appendix C, we approximate the joint characteristic functional (19) according to:
φ [ α ( x ) , β ( x ) , t ] = e 1 2 d x d x α i ( x ) C i j u u ( x ; x , t ) α j ( x ) + 2 α i ( x , t ) C i j u h ( x ; x , t ) β j ( x ) + β i ( x ) C i j h h ( x ; x , t ) β j ( x ) ,
where we introduced the two-point correlation functions (14)–(16). As a consequence, the entire multi-point statistics is determined by the correlation function Equations (14)–(16).

4. Closure of the Single-Point Magnetic Field PDF Equation and the Assumptions of Isotropy and Homogeneity

In this section, we rely on the characteristic functional (27), which was derived under the assumption of vanishing joint cumulants higher than order two. The closure method can thus be considered as a joint Gaussian closure assumption for the velocity and magnetic field. Similar closures were discussed in the context of the multi-point vorticity statistics in two-dimensional turbulence [36], as well as for the PDF of the velocity gradient tensor in three-dimensional turbulence [37]. We reformulate the evolution equation of the single point magnetic field PDF in terms of conditional expectation values:
t f h ( b , x , t ) + x i u i ( x , t ) | b , x , t f h ( b , x , t ) = b i d x δ ( x x ) b n x n u i ( x , t ) | b , x , t f h ( b , x , t ) + λ 2 x n 2 f h ( b , x , t ) λ 2 b i b j h i ( x , t ) x n h j ( x , t ) x n | b , x , t f h ( b , x , t ) ,
where we imply summation over the same indices. Moreover, we defined the conditional expectation values:
u ( x , t ) | b , x , t = u ( x , t ) δ ( b h ( x , t ) ) δ ( b h ( x , t ) ) ,
h i ( x , t ) x n h j ( x , t ) x n | b , x , t = h i ( x , t ) x n h j ( x , t ) x n δ ( b h ( x , t ) ) δ ( b h ( x , t ) ) ,
and made use of the relation:
2 x n 2 f h ( b , x , t ) = b i 2 h i ( x , t ) x n 2 δ ( b h ( x , t ) ) + 2 b i b j h i ( x , t ) x n h j ( x , t ) x n δ ( b h ( x , t ) ) .
As shown in Appendix C, the first conditional expectation value (29) can be calculated from the joint Gaussian characteristic functional according to:
u i ( x , t ) | b , x , t = C i j u h ( x ; x , t ) C j k h h ( x ; x , t ) 1 b k ,
where C j k h h ( x ; x , t ) 1 denotes the inverse of the two-point tensor (16). Furthermore, under the assumption of translational invariance of the fields, we can neglect derivatives of single-point quantities x · , such as the second term on the l.h.s. of Equation (28). In addition, two-point correlations will only depend on the separation vector r = x x . Next to homogeneity, we also want to impose isotropy, i.e., rotational invariance. Here, special attention has to be paid to the fact that unlike u , h is an axial vector. Therefore, correlations that contain an odd number of magnetic field components such as Equation (32) are skew tensors [1,28,38]. Hence, the correlation tensors that enter the conditional expectation values in Equation (32) read:
C i j u h ( r , t ) = C u h ( r , t ) ε i j k r k
C i j h h ( 0 , t ) = h r m s 2 δ i j ,
where h r m s denotes the root mean square magnetic field h 2 . Furthermore, the assumption of isotropy implies that the single-point PDF solely depends on the absolute of the magnetic field b = | b | . This PDF is related to the PDF of the absolute value of the magnetic field f h ( b , t ) according to [39]:
f h ( b , t ) = 4 π b 2 f h ( b , x , t ) .
Therefore, the remaining nonlinear term, i.e., the first term on the r.h.s. of Equation (28), yields:
b · d r δ ( r ) b · r u ( x + r , t ) | b , x , t f h ( b , x , t ) = h r m s 2 b i d r δ ( r ) b n r n C u h ( r , t ) ε i j l r l δ j k b k f h ( b , x , t ) = h r m s 2 d r δ ( r ) C u h ( r , t ) r r n r ε i j l r l + C u h ( r , t ) ε i j n × δ i n b j f h ( b , x , t ) + δ i j b n f h ( b , x , t ) + b j b n b i b f h ( b , x , t ) b = 0 .
where we made use of the general relation r n g ( r ) = g ( r ) r r n r and used the properties of the Levi–Civita tensor, e.g., ε i j l r l r i = 0 and ε i i l = 0 . Remarkably, the joint Gaussian approximation combined with the assumptions of homogeneity and isotropy leads to vanishing nonlinear transfer terms in the single-point PDF equation. In other words, the growth of magnetic field fluctuations (in a setting with translational invariance and no preferred direction) requires non-vanishing higher-order cumulants, e.g., generated by non-vanishing third order moments.
The remaining term involves the conditional expectation value (30), which simplifies to:
h i ( x , t ) x n h j ( x , t ) x n | b , x , t = ε h h 3 λ δ i j ,
where we have introduced the average of the local magnetic energy dissipation rate according to:
ε h h = λ 2 h i ( x , t ) x j + h j ( x , t ) x i 2 .
Consequently, Equation (28) reduces to:
t f ˜ h ( b , t ) = b 2 ε h h 3 b f ˜ h ( b , t ) + 2 b 2 ε h h 3 f ˜ h ( b , t ) ,
Accordingly, taking the second moment of this equation yields the temporal evolution for the magnetic energy:
t E m a g ( t ) = 1 2 d b b 2 t f h ( b , t ) = ε h h .
Due to the vanishing of the nonlinear term in Equation (36), Equation (39) possesses no transfer term, which again is a direct consequence of the isotropy/homogeneity assumption and the neglect of higher order cumulants in the joint characteristic functional (19). A possible way of restoring this missing term within the same joint Gaussian approximation consists of allowing for a mean magnetic field H ( t ) = h ( x , t ) , which fluctuates about the mean direction λ = H ( t ) / H ( t ) t . In this case, we necessarily have to deal with axisymmetric MHD turbulence, and the skew symmetric tensor (33) gets modified to [38]:
C i j u h ( r , t ) = C ( 1 ) ( r , t ) ε i j k r k + C ( 2 ) ( r , t ) λ j ε i l m λ l r m + C ( 3 ) ( r , t ) r j ε i l m λ l r m ,
which allows for a non-vanishing transfer term in Equation (28). As has been reported in numerical [40], theoretical [41] and experimental studies [42] alike, MHD flows can develop strong anisotropies in the presence of a mean magnetic field. This is all the more important as symmetry breaking, e.g., due to shear, apparently is a crucial ingredient for dynamo action in MHD flows [43,44]. The implications of the presence of such mean magnetic fields in the PDF equations, especially in the context of dynamo theory, will be discussed in a forthcoming publication.

5. Discussion

We presented a comprehensive statistical description of MHD turbulence. First, we formulated a hierarchy of evolution equations for multi-point probability density functions that can be considered as the analogon to the multi-point PDF hierarchy derived by Lundgren [24]. In comparison to the latter hierarchy of hydrodynamic turbulence, where unclosed terms are due to pressure and viscous contributions, the Alfvén effect introduces additional unclosed terms. Furthermore, we discussed the relation of the PDF hierarchy to the moment hierarchy of Chandrasekhar [1] and presented a compact formulation on the basis of a joint characteristic functional in MHD turbulence [33]. A joint Gaussian approximation for this characteristic functional has been used in order to close two-point terms in the evolution equation for the single-point magnetic field PDF.
It will be a task for the future to assess these conditional averages by direct numerical simulations, similarly to the case of hydrodynamic turbulence [36,37] and further quantify deviations from Gaussianity and their origin in the dynamics of MHD turbulence. Moreover, it might also be interesting to investigate the implications of Alfvén waves within the PDF framework and to enlarge it possibly in order to account for the effects of stratification. The latter treatment starts directly from the Boussinesq equation and could enhance our current understanding of non-Gaussian features found empirically at the scale of the mean stratified flow [45].

Funding

I acknowledge funding from the Humboldt Foundation within a Feodor-Lynen fellowship. Moreover, I benefited from financial support through the Project IDEXLYONof the University of Lyon in the framework of the French program “Programme Investissements d’Avenir” (ANR-16-IDEX-0005).

Acknowledgments

I want to thank Alain Pumir for interesting discussions.

Conflicts of Interest

The author declares no conflict of interest.

Appendix A. Derivation of the PDF Hierarchy

This Appendix discusses the derivation of the evolution equations for the single-point velocity Equation (9) and magnetic field PDF Equation (11).

Appendix A.1. Terms of the Evolution Equation for the Single-Point Velocity PDF

The first nonlinear term in Equation (1) can be related to the single-point PDF by the following manipulation:
v · u ( x , t ) · x u ( x , t ) δ ( v u ( x , t ) ) = u ( x , t ) · x δ ( v u ( x , t ) ) = x · u ( x , t ) δ ( v u ( x , t ) ) = v · x δ ( v u ( x , t ) ) = f u ( v , x , t ) ,
where we made use of the incompressibility of the velocity field after the second equality and used the so-called sifting property of the δ -distribution, u ( x , t ) δ ( v u ( x , t ) ) = v δ ( v u ( x , t ) ) , after the last equality. The second nonlinear term, however, involves the magnetic field and has to be related to a two-point quantity:
v · h ( x , t ) · x h ( x , t ) δ ( v u ( x , t ) ) = v i [ h n ( x , t ) x n h i ( x , t ) ] δ ( v u ( x , t ) ) = v i d x δ ( x x ) x n h n ( x , t ) h i ( x , t ) δ ( v u ( x , t ) ) = v i d x δ ( x x ) x n d b b n b i δ ( v u ( x , t ) ) δ ( b h ( x , t ) ) f u h ( v , x ; b , x , t ) = v · d x δ ( x x ) d b b · x b f u h ( v , x ; b , x , t ) ,
where we implied summation over equal indices. The next term involves nonlocal pressure contributions and, therefore, again, two-point quantities. The total pressure field can be obtained by taking the divergence of Equation (1), which yields the Poisson equation:
x 2 p ( x , t ) = x · [ u ( x , t ) · x u ( x , t ) h ( x , t ) · x h ( x , t ) ] ,
which can be solved by the usual Green’s function method according to:
p ( x , t ) = 1 4 π d x 1 | x x | x · [ u ( x , t ) · x u ( x , t ) h ( x , t ) · x h ( x , t ) ] ,
where we assumed an infinite domain without further boundary conditions. Accordingly, the pressure term that enters Equation (9) reads:
v · x p ( x , t ) δ ( v u ( x , t ) ) = 1 4 π v · d x x 1 | x x | 2 x i x n u n ( x , t ) u i ( x , t ) h n ( x , t ) h i ( x , t ) δ ( v u ( x , t ) ) = 1 4 π v · d x x 1 | x x | 2 x i x n d v v n v i δ ( v u ( x , t ) ) δ ( v u ( x , t ) ) 1 4 π v · d x x 1 | x x | 2 x i x n d b b n b i δ ( v u ( x , t ) ) δ ( b h ( x , t ) ) = 1 4 π v · d x x 1 | x x | d v v · x 2 f u u ( v , x ; v , x , t ) 1 4 π v · d x x 1 | x x | d b b · x 2 f u h ( v , x ; b , x , t ) .
Finally, the viscous term reads:
ν v · x 2 u ( x , t ) δ ( v u ( x , t ) ) = ν v · d x δ ( x x ) x 2 u ( x , t ) ) δ ( v u ( x , t ) ) = ν v · d x δ ( x x ) x 2 d v v δ ( v u ( x , t ) ) δ ( v u ( x , t ) ) f u u ( v , x ; v , x , t ) ,
Inserting the terms (A1), (A2), (A5), and (A6) into Equation (8) yields the evolution equation for the single-point velocity PDF (9).

Appendix A.2. Terms of the Evolution Equation for the Single-Point Velocity PDF

The first nonlinear term from the induction Equation (2) can be related to a single-point mixed quantity:
b · u ( x , t ) · x h ( x , t ) δ ( b h ( x , t ) ) = u ( x , t ) · x δ ( b h ( x , t ) ) = x · u ( x , t ) δ ( b h ( x , t ) ) = x · d v v δ ( v u ( x , t ) ) δ ( b h ( x , t ) ) = d v v · x f u h ( v , x ; b , x , t ) .
The second term, however, has to be related to the two-point PDF Equation (6) according to:
b · h ( x , t ) · x u ( x , t ) δ ( b h ( x , t ) ) = b i h n ( x , t ) x n u i ( x , t ) δ ( b h ( x , t ) ) = b i d x δ ( x x ) x n h n ( x , t ) u i ( x , t ) δ ( b h ( x , t ) ) = b i d x δ ( x x ) x n d v b n v i δ ( v u ( x , t ) ) δ ( b h ( x , t ) ) = b · d x δ ( x x ) d v b · x v f u h ( v , x ; b , x , t ) .
Finally, the viscous term that enters the evolution equation for the one-point magnetic field PDF can be treated in the same way as Equation (A6).

Appendix B. Relation to the Moment Hierarchy Derived by Chandrasekhar

In this section, we want to derive the evolution equation for the moments (14)–(16) directly from the PDF equations.

Appendix B.1. Evolution Equation for the Two-Point Velocity Field Correlation Tensor

The evolution equation for the two-point velocity PDF (5) can be obtained from the generalized Equation (13) according to:
t + v · x + v · x f u u ( v , x ; v , x , t ) = v · d x δ ( x x ) + v · d x δ ( x x ) d b b · x b f u u h ( v , x ; v , x ; b , x , t ) ν v · d x δ ( x x ) + v · d x δ ( x x ) x 2 d v v f u u u ( v , x ; v , x ; v , x , t ) ,
where we already neglected pressure contributions due to the fact that they vanish on the basis of homogeneity at this stage of the moment hierarchy discussed in the following (nonetheless, they do not vanish for higher order correlations [9]). Taking the moments:
v i ( x , t ) v j ( x , t ) = d v v i d v v j f u u ( v , x ; v , x , t ) ,
of Equation (A9) yields:
t u i ( x , t ) u j ( x , t ) + x n u n ( x , t ) u i ( x , t ) u j ( x , t ) + x n u n ( x , t ) u i ( x , t ) u j ( x , t ) = x n h n ( x , t ) h i ( x , t ) u j ( x , t ) + x n h n ( x , t ) u i ( x , t ) h j ( x , t ) + ν [ x 2 + x 2 ] u i ( x , t ) u j ( x , t ) .
where we performed partial integration with respect to v and v on the r.h.s. of Equation (A9).

Appendix B.2. Evolution Equation for the Two-Point Cross Helicity Correlation Tensor

The evolution equation for the two-point PDF (6) reads:
t + v · x f u h ( v , x ; b , x , t ) + d v v · x f u u h ( v , x ; v , x ; b , x , t ) = v · d x δ ( x x ) d b b · x b f u h h ( v , x ; b , x ; b , x , t ) b · d x δ ( x x ) d v b · x v f u u h ( v , x ; v , x ; b , x , t ) ν v · d x δ ( x x ) x 2 d v v f u u h ( v , x ; v , x ; b , x , t ) λ b · d x δ ( x x ) x 2 d b b f u h h ( v , x ; b , x ; b , x , t ) ,
where we again dropped the pressure contributions. Taking the moments:
u i ( x , t ) h j ( x , t ) = d v v i d b b j f u h ( v , x ; b , x , t ) ,
of Equation (A12) yields:
t u i ( x , t ) h j ( x , t ) + x n u n ( x , t ) u i ( x , t ) h j ( x , t ) + x n u n ( x , t ) u i ( x , t ) h j ( x , t ) = x n h n ( x , t ) h i ( x , t ) h j ( x , t ) + x n h n ( x , t ) u i ( x , t ) u j ( x , t ) + [ ν x 2 + λ x 2 ] u i ( x , t ) h j ( x , t ) .

Appendix B.3. Evolution Equation for the Two-Point Magnetic Field Correlation Tensor

Finally, the evolution equation for the two-point magnetic field PDF (7) reads:
t f h h ( b , x ; b , x , t ) + d v v · x f u h h ( v , x ; b , x ; b , x , t ) + d v v · x f u h h ( v , x ; b , x , b , x , t ) = b · d x δ ( x x ) d v b · x v f u h h ( v , x ; b , x ; b , x , t ) b · d x δ ( x x ) d v b · x v f u h h ( v , x ; b , x ; b , x , t ) λ b · d x δ ( x x ) + b · d x δ ( x x ) x 2 d b b f h h h ( b , x ; b , x ; b , x , t ) .
Taking the moments:
h i ( x , t ) h j ( x , t ) = d b b i d b b j f h h ( b , x ; b , x , t ) ,
of Equation (A15) yields:
t h i ( x , t ) h j ( x , t ) + x n u n ( x , t ) h i ( x , t ) h j ( x , t ) + x n u n ( x , t ) h i ( x , t ) h j ( x , t ) = x n h n ( x , t ) u i ( x , t ) h j ( x , t ) + x n h n ( x , t ) h i ( x , t ) u j ( x , t ) + λ [ x 2 + x 2 ] h i ( x , t ) h j ( x , t ) .

Appendix C. Gaussian Approximation for the Joint Characteristic Functional of the MHD Equations

In this Appendix, we derive a cumulant expansion for the joint characteristic functional (19) and consider the implications of the vanishing of cumulants higher than order two. In order to expand the joint characteristic functional (19) in powers of the fields α ( x ) and β ( x ) , it is convenient to introduce the six-dimensional fields U ( x , t ) = u ( x , t ) h ( x , t ) and γ ( x ) = α ( x ) β ( x ) . We can now expand the characteristic functional (19) in a power series:
ϕ [ γ ( x ) , t ] = e i d x γ ( x ) · U ( x , t ) = ϕ [ 0 ] + d x δ ϕ [ γ ( x ) , t ] δ γ I ( x ) γ ( x ) = 0 γ I ( x ) + 1 2 ! d x d x δ 2 ϕ [ γ ( x ) , t ] δ γ I ( x ) δ γ J ( x ) γ ( x ) = 0 γ I ( x ) γ J ( x ) + h . o . t . = 1 + i d x U I ( x , t ) γ I ( x ) + i 2 2 ! d x d x U I ( x , t ) U J ( x , t ) γ I ( x ) γ J ( x ) + h . o . t . = 1 + n = 1 d x 1 d x n i n n ! γ I 1 ( x 1 ) γ I n ( x n ) C I 1 I n ( x 1 , , x n , t ) ,
where capital indices indicate I = 1 , , 6 and where we implied summation over equal indices. Moreover, we defined the correlation function:
C I 1 I n ( x 1 , , x n , t ) = U I 1 ( x 1 , t ) U I 2 ( x 2 , t ) U I n ( x n , t ) .
On the other hand, we can cast Equation (A18) in terms of the cumulants according to:
ϕ [ γ ( x ) , t ] = exp n = 1 d x 1 d x n i n n ! γ I 1 ( x 1 ) γ I n ( x n ) K I 1 I n ( x 1 , , x n , t ) ,
which suggests that the first four cumulants K are related to the correlations functions C according to:
K I = C I ,
K I J = C I J C I C J ,
K I J L = C I J L C I J C L C I L C J C J L C I + 2 C I C J C L ,
K I J L M = C I J L M C I J C L M C I L C J M C I M C J L C I J L C M C I J M C L C I M L C J C J L M C I + 2 C I J C L C M + 2 C I L C J C M + 2 C I M C J C L + 2 C M L C I C J + 2 C J L C I C M + 2 C J M C I C L 6 C I C J C L C M .
Under the assumption that there are no mean fields, i.e., K i = 0 , and neglecting higher order cumulants (A23) and (A24), etc., we obtain:
ϕ [ γ ( x ) , t ] = e 1 2 d x d x γ I ( x ) K I J ( x ; x , t ) γ J ( x )
Inserting the original fields u ( x , t ) and h ( x , t ) , as well as the correlation functions (14)–(16) thus yields:
φ [ α ( x ) , β ( x ) , t ] = e 1 2 d x d x α i ( x ) C i j u u ( x ; x , t ) α j ( x ) + 2 α i ( x , t ) C i j u h ( x ; x , t ) β j ( x ) + β i ( x ) C i j h h ( x ; x , t ) β j ( x ) .
In order to calculate the conditional expectation value that enters the evolution equation for the single-point magnetic field, we consider the following relation:
u i ( x , t ) δ ( b h ( x , t ) ) = 1 ( 2 π ) 3 d w e i w · b δ ϕ [ α ( x ) , β ( x ) , t ] δ ( i α i ( x ) ) β ( x ) = w δ ( x x ) α ( x ) = 0 .
Inserting the Gaussian approximation of the characteristic functional Equation (A26) yields:
u i ( x , t ) δ ( b h ( x , t ) ) = i ( 2 π ) 3 d w e i w · b C i j u h ( x ; x , t ) w j e i w · h ( x , t ) = C i j u h ( x ; x , t ) b j 1 ( 2 π ) 3 d w e i w · b e i w · h ( x , t ) = C i j u h ( x ; x , t ) b j f h ( b , x , t ) .
Accordingly, the conditional moment (32) can be expressed as:
u i ( x , t ) | b , x , t = C i j u h ( x ; x , t ) C j k h h ( x ; x , t ) 1 b k ,
where C j k h h ( x ; x , t ) 1 denotes the inverse of the two-point tensor (16).

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Friedrich, Jan. 2020. "Probability Density Functions in Homogeneous and Isotropic Magneto-Hydrodynamic Turbulence" Atmosphere 11, no. 4: 382. https://doi.org/10.3390/atmos11040382

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Friedrich, J. (2020). Probability Density Functions in Homogeneous and Isotropic Magneto-Hydrodynamic Turbulence. Atmosphere, 11(4), 382. https://doi.org/10.3390/atmos11040382

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