Evolution of similarity lengths in anisotropic magnetohydrodynamic turbulence
Riddhi Bandyopadhyay, William H. Matthaeus, Sean Oughton, Minping Wan

TL;DR
This paper confirms through simulations that anisotropic MHD turbulence exhibits a steady ratio of parallel to perpendicular similarity lengths during decay, supporting a theoretical similarity solution and revealing a Taylor–Kármán-like decay behavior.
Contribution
The study validates the similarity hypothesis in anisotropic MHD turbulence and demonstrates a steady ratio of length scales during decay using direct numerical simulations.
Findings
The ratio of parallel to perpendicular length scales fluctuates around a steady value.
A Taylor–Kármán-like similarity decay is observed in MHD turbulence.
The parameters like Reynolds number and magnetic field influence the decay behavior.
Abstract
In an earlier paper (Wan et al. 2012), the authors showed that a similarity solution for anisotropic incompressible 3D magnetohydrodynamic (MHD) turbulence, in the presence of a uniform mean magnetic field , exists if the ratio of parallel to perpendicular (with respect to ) similarity length scales remains constant in time. This conjecture appears to be a rather stringent constraint on the dynamics of decay of the energy-containing eddies in MHD turbulence. However, we show here, using direct numerical simulations, that this hypothesis is indeed satisfied in incompressible MHD turbulence. After an initial transient period, the ratio of parallel to perpendicular length scales fluctuates around a steady value during the decay of the eddies. We show further that a Taylor--K\'arm\'an-like similarity decay holds for MHD turbulence in the presence of a mean magnetic field. The…
| Simulation | ||||||
|---|---|---|---|---|---|---|
| run0 | 0.5 | 0.002 | 0.0 | 1.0 | 0.001 | |
| run1 | 1 | 0.002 | 0.0 | 1.0 | 0.001 | |
| run2 | 1 | 0.002 | 0.5 | 1.0 | 0.001 | |
| run3 | 1 | 0.002 | 0.0 | 0.5 | 0.001 | |
| run4 | 2 | 0.002 | 0.0 | 1.0 | 0.0005 | |
| run5 | 3 | 0.002 | 0.0 | 1.0 | 0.0004 | |
| run6 | 2 | 0.002 | -0.5 | 1.0 | 0.0005 | |
| run7 | 4 | 0.002 | 0.0 | 1.0 | 0.00025 | |
| run8 | 2 | 0.002 | 0.0 | 2.0 | 0.0005 | |
| run9 | 2 | 0.002 | 0.8 | 2.0 | 0.0005 | |
| run10 | 1 | 0.0005 | 0.0 | 1.0 | 0.0005 | |
| run11 | 0 | 0.002 | 0.5 | 1.0 | 0.0005 |
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Evolution of similarity lengths in anisotropic
magnetohydrodynamic turbulence
Riddhi Bandyopadhyay
\aff1,2 \corresp William H. Matthaeus
\aff1,2 Sean Oughton
\aff3
Minping Wan\aff4
\aff1 Department of Physics and Astronomy, University of Delaware, Newark, DE 19716, USA \aff2 Bartol Research Institute, University of Delaware, Newark, DE 19716, USA \aff3 Department of Mathematics and Statistics, University of Waikato, Hamilton 3240, NZ \aff4 Department of Mechanics and Aerospace Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, People’s Republic of China
Abstract
In an earlier paper (Wan et al., 2012), the authors showed that a similarity solution for anisotropic incompressible 3D magnetohydrodynamic (MHD) turbulence, in the presence of a uniform mean magnetic field , exists if the ratio of parallel to perpendicular (with respect to ) similarity length scales remains constant in time. This conjecture appears to be a rather stringent constraint on the dynamics of decay of the energy-containing eddies in MHD turbulence. However, we show here, using direct numerical simulations, that this hypothesis is indeed satisfied in incompressible MHD turbulence. After an initial transient period, the ratio of parallel to perpendicular length scales fluctuates around a steady value during the decay of the eddies. We show further that a Taylor–Kármán-like similarity decay holds for MHD turbulence in the presence of a mean magnetic field. The effect of different parameters, including Reynolds number, DC field strength, and cross-helicity, on the nature of similarity decay is discussed.
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1 Introduction
Turbulence is a ubiquitous phenomenon that spans a broad range of temporal and spatial scales. In a turbulent system energy is transferred from large (or “energy-containing”) eddies to small eddies, ultimately resulting in production of internal energy or heat by dissipation. This process of energy cascade is observed in turbulent neutral fluids as well as turbulent plasmas. The rate of energy decay in a turbulent system is both an interesting problem (Kolmogorov, 1941) and also an important practical one. In laminar flows the rate of energy loss is determined by the molecular viscosity of the fluid, but in a turbulent system the energy dissipation rate appears to become independent of viscosity and approach a non-zero value as the fluid becomes increasingly turbulent (Onsager, 1949). Taylor (1938) gave an empirical expression for the energy decay rate of turbulent neutral fluids. This analytical expression can be obtained from the work of von Kármán & Howarth (1938) by assuming the preservation of the shape of the two-point correlation function during turbulent decay (Dryden, 1943).
Energy decay in plasmas is a more complicated problem. Magnetohydrodynamic (MHD) theory is the simplest extension of hydrodynamic turbulence theories to conducting fluids and the decay of energy-containing eddies in MHD turbulence has been the subject of various studies (e.g., Hossain et al., 1995, 1996; Linkmann et al., 2015, 2017). Note that the presence of an external mean magnetic field, , makes the problem of energy decay in MHD more complex because the mean field introduces anisotropy in the system (Robinson & Rusbridge, 1971; Montgomery & Turner, 1981; Montgomery, 1982; Shebalin et al., 1983; Oughton et al., 1994; Hossain et al., 1995).
Energy cascade through the MHD inertial scales is given by a Kolmogorov–Yaglom (Kolmogorov, 1941; Monin & Yaglom, 1975) third-order law extended to MHD (Politano & Pouquet, 1998a, b). On average, the energy transfer rate associated with cascading of excitation from the large scales (determined by the von Kármán-type phenomenology) and the energy cascade rate associated with inertial range scales (given by the third-order law) are expected to be in agreement (Kolmogorov, 1941; Batchelor, 1953; Bandyopadhyay et al., 2018).
The problem of similarity decay in isotropic and anisotropic incompressible MHD turbulence is studied in detail by Wan et al. (2012), where it is shown that similarity solutions are possible in MHD. However, unlike the situation for isotropic neutral fluids, universality, even at asymptotically high Reynolds number, is not expected for MHD due to potential variation of other parameters such as magnetic Prandtl number, cross helicity, magnetic helicity, and Alfvén ratio. Thus one might anticipate that in MHD the conditions for obtaining similarity solutions are more restrictive. Indeed, Wan et al. (2012) shows, analytically, that a similarity solution for MHD fluid with a mean magnetic field is possible only if, during the similarity decay, the similarity length scale parallel to the mean field remains proportional to the similarity length scale perpendicular to the mean field. As far as we are aware, whether the two length scales remain in constant proportion has not yet been tested in simulations or experiments. This motivates the present study. We will discuss results from a set of (spectral method) numerical experiments of MHD turbulence that examine the dynamical behaviour of the ratio of the parallel and perpendicular correlation scales. This enables us to assess whether or not a similarity decay phase occurs in anisotropic 3D MHD in the presence of a DC magnetic field (Wan et al., 2012). The results confirm, perhaps surprisingly, that the required condition for similarity decay of anisotropic MHD can be satisfied.
2 Theory
In this section we briefly review the Wan et al. (2012) derivation of similarity decay phenomenology for anisotropic MHD with a mean magnetic field. As in that work, we take the mass density to be constant and set it to unity. We denote the fluctuating velocity and magnetic fields by and , respectively. Without loss of generality, we take the mean magnetic field as . All magnetic fields are converted to Alfvén units. The equations of incompressible MHD can be written in terms of Elsasser variables for the fluctuations, , as
[TABLE]
where is the total (magnetic+kinetic) pressure, and is the viscosity, for simplicity assumed to be equal to the resistivity herein.
The second-order correlation tensors for the corresponding Elsasser fields are defined as
[TABLE]
where denotes an ensemble average. Using the MHD equations one can derive the following equation for the time evolution of the traced second-order correlation function,
[TABLE]
Here
[TABLE]
is a triple correlation. Interestingly, the mean magnetic field does not appear explicitly in (3), despite the well-known fact that these correlation functions (and their Fourier transforms, the Elsasser energy spectra) do display anisotropy relative to . In fact, the first explicit appearance of a DC magnetic field in the correlation function hierarchy is in the equation for evolution of the third-order correlations (Wan et al., 2012; Oughton et al., 2013). Consequently, the dynamical influence of is exerted on (3) through the structure of the third-order correlations. Therefore, the limit of large that permits reduction to quasi-2D MHD must occur in those higher order equations, and not directly in (3).
A set of similarity solutions can be derived from these equations using a heuristic scaling argument, as shown by von Kármán & Howarth (1938) for hydrodynamic turbulence and generalized to MHD by Wan et al. (2012). Here, we outline the steps only for the case of anisotropic MHD decay in the presence of a mean magnetic field. It is well established that a mean magnetic field affects the dynamics of the dissipation rate in a turbulent system (e.g., Shebalin et al., 1983; Oughton et al., 1994; Bigot et al., 2008a, b). Without loss of generality, we allow for non-zero cross helicity . The zero cross-helicity case is recovered as a special solution.
Assuming the system to be axisymmetric with respect to the mean field direction , we write the second-order correlation functions in the form
[TABLE]
where and . Clearly, and are equivalent to the height and radial coordinates in the usual cylindrical polar coordinate system . Using the theory of axisymmetric tensors (Batchelor, 1953; Politano et al., 2003), the triple correlations can be written as
[TABLE]
Inserting expressions (6)–(7) into (3) yields
[TABLE]
where
[TABLE]
with and .
Following von Kármán & Howarth (1938) and Wan et al. (2012) we assume
[TABLE]
introducing the normalized variables and , and the shorthand notation .
Using (11)–(13), in (8) we obtain
[TABLE]
where . We assume here that the “” and “” variables are independent of each other. For ease of identification we have written all the terms that are explicitly dependent on time inside curly brackets: . Terms that do not explicitly depend on time are written inside square brackets: . There are two points to note here. First, because and are functions of time, the square-bracketed terms will in general have implicit time dependence. Second, a priori one would expect the variable to be time dependent. Thus, the claim that the square-bracketed terms lack explicit time dependence will only be true if is constant. The dynamical relevance of this constraint is the primary focus of this study.
As an aside, we note that this requirement for similarity solutions may not pertain to the asymptotic case of , i.e., . In this circumstance, the fourth term of (14) can be separated into a time-dependent part and a time-independent part, regardless of the behaviour of , in the asymptotic limit. Physically, this limit would be relevant to phenomena or structures that are strongly elongated along the parallel direction. A similarity solution might then exist without the need for constant.
Without pursuing the above mentioned limits here, and assuming that remains constant in time, we can gather all the terms inside curly brackets in (14) and set them proportional to each other. Proceeding accordingly, we can write
[TABLE]
so that
[TABLE]
where and are both positive time-independent constants. In deriving (16)–(17) we have ignored the terms containing the viscosity in (14), due to the assumption ; i.e., high Reynolds number. The “” versions of (14)–(17) are analogous.
Equations (16) and (17) can be heuristically derived from dimensional analysis and modelling (e.g., Dobrowolny et al., 1980; Hossain et al., 1995; Biskamp & Schwarz, 2001). The derivation presented here and in Wan et al. (2012) highlights the underlying assumptions and limitations of these solutions. For example, the derivation relies on the assumption of similarity, i.e., that the two-point correlation function maintains its shape during the decay. Moreover, the requirement that needs to remain constant in time is manifested through this analysis.
Equations (16) and (17) are exactly satisfied if the solutions obey the conservation law
[TABLE]
For the long time behaviour of and , one expects, on the basis of physical arguments for decaying turbulence (Matthaeus et al., 1996), that
[TABLE]
We now test these hypotheses using spectral simulations.
3 Simulations
To test the hypothesis that the Elsasser energies and correlation lengths of (unforced) MHD turbulence evolve according to von Kármán–Howarth similarity decay laws—equations (16)–(17) and their ‘minus’ partners—and which also requires that the ratio of the parallel and perpendicular characteristic lengths does not change in time, we carry out a set of incompressible MHD simulations with a mean magnetic field, .
All runs are initialized with kinetic and magnetic spectra proportional to , with and only the Fourier modes within the band excited. The initial total energy is always normalized to one. Correlation lengths are small compared to the total box length for all runs. Table 1 contains a summary of the simulation parameters used for this study. Although we are here mainly concerned with anisotropy induced by a DC magnetic field, for context we also include results from an isotropic simulation that lacks a global DC field (run11).
We numerically solve (1) in a periodic box using a pseudo-spectral solver without any external forcing. All the variables are expanded in a Fourier basis with transfer between real space and Fourier space performed using a Fast Fourier Transform (FFT). We use the second-order Runge–Kutta (RK2) scheme for time-stepping, and the rule for dealiasing. To ensure accuracy of the dissipation rates and spectra we require that for all simulations (Wan et al., 2010; Donzis et al., 2008). Here is the maximum resolved wavenumber and is the Kolmogorov dissipation length scale.
For strong mean field, the simulations can be performed in non-cubic boxes, provided the parallel cascade (in addition to the perpendicular cascade) is well resolved (Oughton et al., 2004). For a well-resolved case, a non-cubic simulation domain is not expected to modify the dynamics in incompressible MHD (Bigot et al., 2008b). We employ a cubic periodic box for all runs discussed herein.
4 Results
To study the decay dynamics of the energy-containing eddies we compute, at each timestep, the “Elsasser energies” and and their characteristic lengths along each Cartesian coordinate direction. The latter are calculated from the two-point correlation functions (see (2)) as
[TABLE]
and similarly for the and components. Here, are the trace of the correlation tensors. In Fourier space, we can equivalently define the length scales as
[TABLE]
So, the length scales are proportional to the reduced spectrum evaluated at zero wavenumber: . We define
[TABLE]
The factor of in the definition of is used because there are two independent components in the perpendicular plane (e.g., Oughton & Matthaeus, 2005). With this definition we usefully have for the isotropic case, when .
Figure 1 shows the time histories of the total fluctuation energy (magnetickinetic), Elsasser energies , mean energy dissipation rate , and fluid Reynolds number for all the runs in table 1. Note that these quantities are associated with the fluctuations and, in particular, the calculation of Elsasser variables, their energies, and the total fluctuation energy does not include the contribution from the DC magnetic field, .
Here, is the vorticity and is the current density. The time axis is plotted in units of the initial nonlinear time or “eddy turnover” time, . We employ the following definition for the initial eddy turnover time
[TABLE]
where are the initial correlation lengths, and
[TABLE]
These are straightforward MHD generalisations of the classical definition of the correlation length or integral scale (Batchelor, 1953; Linkmann et al., 2015; Bandyopadhyay et al., 2018b)
[TABLE]
Note that we do not recover the directional length scales of (20, 21) by simply replacing with in (25). The fluid Reynolds number is defined as , where denotes the (average) component rms speed with . Here, is the modal kinetic energy spectrum and is the total kinetic energy.
Panels (a) and (b) of figure 1 indicate that, for all runs considered, a powerlaw (in time) is a reasonable approximation to the decay of both the total fluctuation energy and the Elsasser energies, after a few nonlinear times. This behaviour is expected for von Kármán-Howarth similarity decay (Matthaeus et al., 1996). Not all runs have the identical power-law slope and a full explanations for these slight differences is yet to be obtained. However, it is clear that the decay is (approximately) self-similar at these later times. During these periods the dissipation rates are much smaller than the peak values but are also only slowly decreasing; the Reynolds numbers are also slowly decreasing (with oscillations).
Figure 2 illustrates the time history of the ratio of the parallel to perpendicular length scales , corresponding to the “” Elsasser variable.
It is evident that after an initial transient period, the ratio of the two lengthscales typically saturates to an approximately steady value, with fluctuations around those values.
A closer inspection of figure 1 and figure 2 reveals that the dissipation rate reaches its maximum near unit nonlinear time. However, values saturate at a somewhat later time . This behaviour can probably be explained by noting that modifying the very large lengthscales takes a long time. The correlation lengths may become steady after the lowest wavenumber part of the spectrum is well populated. Since dissipation involves high wavenumber regions of the spectrum, where the characteristics timescales are much faster than those of the energy-containing eddies, it is perhaps not surprising that the dissipation rate peaks before saturates.
Although attains different values for different simulation sets, figure 2 indicates that for all cases remains approximately stationary for many nonlinear times. Furthermore, for the nonzero mean field cases, is always greater than , indicating that the correlation lengths along the mean field are longer than those perpendicular to it, due to the cascade preferentially transferring energy in the perpendicular directions (Shebalin et al., 1983; Grappin, 1986; Matthaeus et al., 1990; Oughton et al., 1994; Goldreich & Sridhar, 1995; Teaca et al., 2009).
Figure 2 contains the main results of this paper. (Plots for , not shown, are completely analogous.) Having established that the ratio of parallel to perpendicular length scales remain (roughly) constant in time, we proceed to examine whether the proposed von Kármán similarity decay is satisfied for MHD fluids in the presence of a global magnetic field.
In figure 3, we show the two “von Kármán constants” and , corresponding to the “” Elsasser variables, as functions of time. If the similarity decay hypothesis is indeed satisfied, these two quantities should maintain constant values in time. Figure 3(a) shows the rate of change of perpendicular length scale normalized to , which, if the decay obeys a similarity solution is a constant, . Panel (b) plots the (negative) normalized rate of change of as a function of time; again, if the decay obeys a similarity this will be a constant, . A central difference scheme is used to evaluate the time derivatives. It is clear from the two panels of figure 3 that the similarity decay hypothesis, as proposed in Wan et al. (2012), is well supported by the simulation results presented here.
Recall also, from equation (18), that the conserved quantity associated with the self-similar decay depends on the ratio . This ratio is displayed in panel (c) of figure 3 where it can be seen that it attains a steady-state value of somewhat less than unity, after an initial adjustment phase. From Dryden (1943) and von Kármán & Lin (1949) self-similar decay for all scales requires . This situation corresponds to the case of decay with constant turbulent viscosity, constant, or equivalently decay at constant Reynolds number. Clearly, this is not satisfied rigorously in the simulations presented here. Further, the plotted values of appear to eliminate the possibility of similarity decay with constant, physically corresponding to the case of constant area under the correlation function. Although only the “” Elsasser variables are shown here, the results are similar for the “” Elsasser variables. As an aside we note that applications of MHD decay phenomenologies within studies of the transport of solar wind fluctuations (e.g., Matthaeus et al., 1996; Zank et al., 1996, and many subsequent papers) have previously employed both the and the conditions.
Next, we briefly discuss the effect of anisotropy due to the DC magnetic field strength and/or the cross-helicity strength. Of particular interest here is the variation of with and with the magnitude of the initial normalized cross-helicity . Figure 4 shows the asymptotic values of for all the runs. These asymptotic values, denoted , are obtained by averaging over the final five nonlinear times for each run. Within the limited parameter range scan of and covered by the simulations presented here, it appears that initially increases with but the effect then saturates for higher values of . This behaviour is expected since the mean-field induced anisotropy renders the system approximately two-dimensional; i.e. . On the other hand, from panel (b) of figure 4, no clear scaling can be deduced between and .
A related quantity of interest is the ratio of the length scales corresponding to the and Elsasser variables. The bottom two panels of figure 4 illustrate the variation of the ratio . Again, the reported values are the temporal averages over the final five nonlinear time units. Here, we see that there is no evident scaling with the mean-field strength . However, panel (d) exhibits a rough increasing scaling of with . This result is consistent with the explanation provided by Matthaeus et al. (1983) and Ghosh et al. (1988), who argue that for high cross-helicity (say, positive), one of the Elsasser fields is weak and it is almost passively advected towards high wavenumber by the dominant Elsasser field . This kind of tendency would result in dissimilar values of the two Elsasser field length scales . From figure 4, the zero cross-helicity runs, run 0, 1, 3, 4, 5, 7, 8, 10, maintain . The positive cross-helicity runs, run 2, 9, 11, show , with increasing value of as increases. Run 6 has and consequently for this case.
5 Discussion
We have examined the validity of a von Kármán–Howarth-like similarity decay phase in anisotropic 3D MHD in the presence of an externally supported DC magnetic field (), as derived in Wan et al. (2012). An analytic result is that a similarity decay phase is only followed in an MHD fluid (with a ) if the ratio of the parallel to perpendicular characteristic lengthscales, , remains constant in time. Using numerical simulations, performed with a range of different parameters, we find that the ratio of parallel to perpendicular length scales does indeed maintain an approximately steady value during the decay of the MHD turbulence, after an initial build-up phase. This result provides substantial support for the occurrence of similarity decay of energy in MHD turbulence with a mean field.
Additionally, since the ratio of the parallel and perpendicular lengthscales maintains a constant value this implies that only one of the lengthscales evolves independently. This has useful consequences for global turbulence-based modelling of the solar wind and other astrophysical plasmas. Often in such models a von Kármán-like phenomenology is invoked (e.g., Breech et al., 2008; Oughton et al., 2011; Usmanov et al., 2014). If the parallel and perpendicular lengths maintain a constant proportion in the solar wind, it may be sufficient to evolve the lengthscale along only one direction, simplifying the calculations and possibly making the computations less expensive.
The results presented in this paper are important for understanding heating and acceleration of space plasmas such as the solar corona, solar wind, and magnetospheric plasmas. The conclusions should also be useful for understanding and modelling the role of turbulence in the evolution and dynamics of astrophysical plasmas and laboratory plasmas.
We note that although the runs have the same initial conditions, after a few nonlinear times they evolve independently to distinct states. Therefore, we suggest that the result, that maintains a steady value, does not depend on the large-scale eddies being of the same form in the parallel and perpendicular directions.
The applicability of the theory for modest Reynolds number warrants some discussion. To arrive at (16) and (17), we neglect the two terms proportional to in (14). This step can be justified by a simple calculation to estimate the order of magnitude of the neglected terms compared to the retained terms in (14). Let us compare the two terms and . For simplicity, we ignore the notations , , , etc., and assume . Then, we can compare the two terms as
[TABLE]
For a consistency check, if we insert the desired solution, , on the LHS we obtain
[TABLE]
Noting that this yields
[TABLE]
So, from this very crude argument, the theory is expected to hold for . In practice, one finds that the conditions for a similarity decay law are much less stringent than, say, the conditions for the Kolmogorv slope (von Kármán & Lin, 1949). In the simulations shown here, the lowest value of Reynolds number is around fifty, . Therefore, in the worst case scenario, the neglected terms are about times smaller than the retained terms in (14). It is clear from the results that this level of smallness for the terms proportional to is sufficient to satisfy an approximate similarity decay.
However, we can infer the effect of Reynolds number and large-scale eddy strength by examining results from two simulations, run 3 and run 10. These differ only by Reynolds number with run 10 having the larger . From figure 4, run 3 has a higher value of (i.e., asymptotic ). One factor contributing to the different values of is probably the different grid size in the two simulations. Further, it is known that mean-field-induced anisotropy depends on Reynolds number, so that may play a role here. The ratio , on the other hand, admits almost equal values for the two runs, presumably since the cross-helicity is the same for both cases. The ‘energy’ similarity decay constant, , expectedly, decreases from run 3 to run 10, due to increased (Linkmann et al., 2015, 2017; Bandyopadhyay et al., 2018b). However, the ‘lengthscale’ similarity constant, , appears to be less sensitive to Reynolds number.
Interestingly, Kármán–Howarth-like similarity decay has been observed in 2DMHD (Biskamp & Schwarz, 2001). However, a comparison of similarity solutions in 2DMHD (or 2.5D MHD) and strong-mean-field 3DMHD is not entirely straightforward since 2DMHD also admits an inverse cascade of mean-squared magnetic potential, . This requires that some magnetic energy is also inverse cascaded and is thus not available for direct cascade to the dissipative small scales. Exploring that parameter space is beyond the scope of the current paper. In particular, the 2D runs would need to scan ( is the energy) and the 3D “comparison” runs would require a scan of , as well as varying the initial polarization (2D versus “2.5D”).
Further, using fully kinetic Particle-In-Cell (PIC) simulations, it has been shown that weakly collisional plasmas support similarity decay (Wu et al., 2013; Parashar et al., 2015). It will be interesting to extend and test the similarity decay phenomenologies discussed here to three-dimensional kinetic simulations, shear driven flows, compressible plasmas, etc. It is not clear why the quantity attains a constant value. Other types of turbulent flow that develop anisotropy, due to rotation, stratification, convection, etc., may also admit a similar stabilization of the ratio of the parallel and perpendicular length scales. Another interesting direction in which the similarity solution can be extended is quasi-static MHD turbulence (see Verma (2017) for a review). We plan to take up these endeavours in the future.
Acknowledgments
This research is supported by NASA under grant NNX17AB79G, and Heliospheric Supporting Research grants 80NSSC18K1210, and 80NSSC18K1648, as well as the Parker Solar Probe Project under Princeton subcontract SUB000016S. The simulations were performed using the Dante and Casella clusters at the University of Delaware, USA.
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