1. Introduction
Wave turbulence theory describes a set of random waves in weakly nonlinear interactions (Zakharov, L'Vov & Falkovich Reference Zakharov, L'Vov and Falkovich1992; Nazarenko Reference Nazarenko2011; Galtier Reference Galtier2023). The strength of this theory, based on a multiple-scale technique, lies in its analytical and rigorous character, and the fact that it leads to a natural asymptotic closure of the hierarchy of moment equations when considering the long-term statistical behaviour. We are interested here in waves resulting from the rapid rotation, at a rate $\varOmega$, of an incompressible fluid: these are inertial waves. They appear when the Coriolis force is introduced into the Navier–Stokes equations, which breaks the spherical symmetry and introduces (statistical) anisotropy. The theory of inertial wave turbulence was derived by Galtier (Reference Galtier2003). It is an asymptotic theory valid in the limit of small Rossby number $R_o = U / (L \varOmega ) \ll 1$, with $U$ a typical velocity and $L$ a typical length scale. The theory, developed for three-wave interactions, predicts anisotropic turbulence with a direct cascade preferentially in the direction transverse to the axis of rotation $\boldsymbol {\varOmega }$. In the limit $k_\perp \gg k_\|$, where $k_\perp$ and $k_\|$ refer to the wavenumbers perpendicular and parallel to $\boldsymbol {\varOmega }$, respectively, an exact solution is derived, the Kolmogorov–Zakharov (KZ) energy spectrum, which is $E_k \sim k_\perp ^{-5/2} \vert k_\| \vert ^{-1/2}$. This solution corresponds to a stationary state for which the energy flux is constant and positive. Note that there is another type of solution, the Rayleigh–Jeans spectrum associated with the thermodynamic equilibrium of the system and for which the energy flux is zero.
Rotating hydrodynamic turbulence has been extensively studied both numerically (Bellet et al. Reference Bellet, Godeferd, Scott and Cambon2006; Pouquet & Mininni Reference Pouquet and Mininni2010; Pouquet et al. Reference Pouquet, Sen, Rosenberg, Mininni and Baerenzung2013; Le Reun et al. Reference Le Reun, Favier, Barker and Le Bars2017; Buzzicotti et al. Reference Buzzicotti, Aluie, Biferale and Linkmann2018; Seshasayanan & Alexakis Reference Seshasayanan and Alexakis2018; Sharma, Verma & Chakraborty Reference Sharma, Verma and Chakraborty2019; van Kan & Alexakis Reference van Kan and Alexakis2020) and experimentally (Baroud et al. Reference Baroud, Plapp, She and Swinney2002; Morize, Moisy & Rabaud Reference Morize, Moisy and Rabaud2005; van Bokhoven et al. Reference van Bokhoven, Clercx, van Heijst and Trieling2009; Lamriben, Cortet & Moisy Reference Lamriben, Cortet and Moisy2011; Campagne et al. Reference Campagne, Gallet, Moisy and Cortet2014; Yarom & Sharon Reference Yarom and Sharon2014; Godeferd & Moisy Reference Godeferd and Moisy2015; Yarom, Salhov & Sharon Reference Yarom, Salhov and Sharon2017). In particular, recent studies (Le Reun, Favier & Le Bars Reference Le Reun, Favier and Le Bars2020; Monsalve et al. Reference Monsalve, Brunet, Gallet and Cortet2020; Yokoyama & Takaoka Reference Yokoyama and Takaoka2021) have reported energy spectra consistent with the prediction of inertial wave turbulence theory. But until now, an important theoretical point has been left out: the verification of the locality of the KZ spectrum to ensure the finiteness of the energy flux. This is a criterion of locality of interactions that supports Kolmogorov's idea that the inertial range is independent of the largest (forcing) and smallest (dissipation) scales. To prove the locality of the KZ spectrum, it is necessary to return to the kinetic equation and study the convergence of the integrals (Zakharov et al. Reference Zakharov, L'Vov and Falkovich1992); this is the first objective of this article. The second objective is to study the energy flux to find an estimate of the Kolmogorov constant.
After a brief introduction to inertial wave turbulence in § 2, we prove that the KZ spectrum is indeed ‘local’, which gives strong theoretical support to recent numerical and experimental studies. In § 3, we show numerically that the energy fluxes in the perpendicular and parallel directions do not behave in the same way because in the latter case some triadic interactions can have a negative contribution to the energy flux, whereas in the former case all interactions contribute to a positive flux. We also numerically estimate the Kolmogorov constant before concluding in § 4.
2. Locality conditions
2.1. Kinetic equation and KZ spectrum
The inviscid equations for incompressible flows in a rotating frame read
where $\boldsymbol {u}$ is a solenoidal velocity ($\boldsymbol {\nabla } \boldsymbol {\cdot }{\,\boldsymbol {u}}=0$), $\boldsymbol {w} = \boldsymbol {\nabla } \times {\boldsymbol {u}}$ is the vorticity and $\boldsymbol {\varOmega } = \varOmega \hat {\boldsymbol {e}}_\|$ ($\vert \hat {\boldsymbol {e}}_\| \vert =1$) is the constant rotation rate. The linear solutions of (2.1) are inertial waves with the angular frequency
The first main result of the theory of inertial wave turbulence is the derivation of the kinetic equation that describes the nonlinear evolution of the energy spectrum on a time scale much larger than the wave period $\tau \sim 1/\omega _k$. For reasons of simplicity, we assume an equipartition of energy densities between the co- and counter-propagating inertial waves, and therefore we do not consider the kinetic helicity, which is then zero. This turbulence being anisotropic with a transfer mainly in the transverse direction to $\boldsymbol {\varOmega }$, it is relevant to write the kinetic equation in the limit $k_\perp \gg k_\|$. Note that we often implicitly assume that the energy is initially isotropically distributed at the largest scales of the system, but the same dynamics is expected if initially the energy is located elsewhere, as long as the inertial wave turbulence condition on the time scales is satisfied (see discussion in Galtier (Reference Galtier2003)). The exception is when the energy is confined to $k_\|=0$, which cannot be described by wave turbulence. In the limit $k_\perp \gg k_\|$, the kinetic equation reads (for more details, see Galtier (Reference Galtier2003))
Here $E_k = E(k_\perp,k_\parallel )$ is the axisymmetric energy spectrum, $s_i$ is the wave polarity ($s_i =\pm 1$ with $i=k,p,q$), $\theta$ is the angle between $\boldsymbol {k}_\perp$ and $\boldsymbol {p}_\perp$ in the triangle $\boldsymbol {k}_\perp + \boldsymbol {p}_\perp + \boldsymbol {q}_\perp = \boldsymbol {0}$, $\delta$ is the Dirac distribution, and the integration in the perpendicular direction is done over the domain $\varDelta _\perp$, which satisfies the previous triadic relation. The integral is preceded by a factor $\epsilon ^2$, with $\epsilon$ a small dimensionless parameter ($0 < \epsilon \ll 1$), which can be identified as the Rossby number (which also means that $w \ll \varOmega$). This means that the nonlinear dynamics develops on a time scale $\sim \tau /\epsilon ^2$, which is much longer than the wave period. The stationary solution of the kinetic equation (2.3) is the KZ spectrum
where $C_E$ is necessarily positive (it will be defined later).
2.2. Convergence domain
We begin with a proposition.
Proposition 2.1 The domain of convergence of the kinetic equation (2.3) for power-law spectra $E_k \sim k_\perp ^{-x} \vert k_\| \vert ^{-y}$ is given by the locality conditions
both of which must be satisfied. This result shows a familiar property of wave turbulence: the KZ spectrum, for which $x=5/2$ and $y=1/2$, falls exactly in the middle of the convergence domain (see figure 1 for an illustration).
Proof. Starting from (2.3), we seek solutions of the form $E_k = C_E k_\perp ^{-x} \vert k_\| \vert ^{-y}$ and introduce the dimensionless variables $\tilde {p}_\perp = p_\perp k_\perp ^{-1}$, $\tilde {q}_\perp = q_\perp k_\perp ^{-1}$, $\tilde {p}_\| = p_\| k_\|^{-1}$ and $\tilde {q}_\| = q_\| k_\|^{-1}$. After integration over the parallel wavenumbers, by taking advantage of the following Dirac distribution property,
to find
one gets
where $\sin \theta = \sqrt {1 - (1 + \tilde {p}_\perp ^2 - \tilde {q}_\perp ^2 )^2 (2 \tilde {p}_\perp )^{-2}}$. There are three regions where the triadic interactions are non-local (regions A, B and C in figure 2) and therefore where convergence of the integrals in expression (2.9) must be checked. We now establish the convergence criteria for each of these three regions.
2.2.1. Region A
We define $\tilde {p}_\perp = 1 + r \cos \beta$ and $\tilde {q}_\perp = r \sin \beta$, with $r \ll 1$ and $\beta \in [{\rm \pi} /4, 3 {\rm \pi}/4 ]$ the polar coordinates with their origin at $(\tilde {p}_\perp, \tilde {q}_\perp )=(1,0)$. Two cases must be distinguished: $s_k=s_p$ and $s_k=-s_p$. An evaluation (to leading order) of the different terms of the integral (2.9) is given in table 1. Note that these evaluations take into account the possible cancellation of the integral due to $\beta$ symmetry.
When $s_k=s_p$, the criterion for convergence of the kinetic equation (2.9) will be given by the following integral:
Therefore, there is convergence if $x+2y < 4$.
When $s_k=-s_p$, we have
and convergence is obtained if $x + y < 6$.
2.2.2. Region B
We define $\tilde {p}_\perp = r \cos \beta$ and $\tilde {q}_\perp = 1+ r \sin \beta$, with this time $\beta \in [-{\rm \pi} /4, {\rm \pi}/4 ]$ the polar coordinates with their origin at $(\tilde {p}_\perp, \tilde {q}_\perp )=(0,1)$. We have two cases: $s_k=s_q$ and $s_k=-s_q$. An evaluation (to leading order) of the different terms of the integral (2.9) is given in table 2. Note that these evaluations take into account the possible cancellation of the integral due to $\beta$ symmetry.
When $s_k=s_q$, the criterion for convergence of the kinetic equation (2.9) will be given by the following integral:
Therefore, there is convergence if $x+2y < 4$.
When $s_k=-s_q$, we have
and convergence is obtained if $x + y < 4$.
2.2.3. Region C
We define $\tilde {p}_\perp = (\tau _2-\tau _1)/2$ and $\tilde {q}_\perp = (\tau _1+\tau _2)/2$, with $-1 \le \tau _1 \le 1$ and $1 \ll \tau _2$. We have two cases: $s_p=s_q$ and $s_p=-s_q$. An evaluation (to leading order) of the different terms of the integral (2.9) is given in table 3. Note that these evaluations take into account the possible cancellation of the integral due to $\tau _1$ symmetry.
When $s_p=s_q$, the criterion for convergence of the kinetic equation (2.9) will be given by the following integral:
Therefore, there is convergence if $3 < x + 2y$.
When $s_p=-s_q$, we have
and convergence is obtained if $2 < x + y$.
In conclusion, a solution is local if the following two conditions are satisfied:
3. Kolmogorov constant
The KZ spectrum is particularly interesting because the associated constant flux allows one to measure the so-called Kolmogorov constant $C_K$. To do so, and following Zakharov et al. (Reference Zakharov, L'Vov and Falkovich1992), we introduce the axisymmetric fluxes
and the power-law energy spectrum $E_k = C_E k_\perp ^{-x} \vert k_\| \vert ^{-y}$ (we only consider the region $k_\| > 0$). With the dimensionless variables introduced in the previous section, we find after applying the Kuznetsov–Zakharov transformation (see § 3.3 in Zakharov et al. (Reference Zakharov, L'Vov and Falkovich1992))
with
After integration, and taking the limit $( x, y ) \rightarrow ( 5/2, 1/2 )$, the flux becomes constant and equal to $\varPi _\perp ^{KZ}$ and $\varPi _\|^{KZ}$. Thanks to L'Hospital's rule, we obtain
where
The ratio between the two fluxes $\varPi _\|^{KZ} / \varPi _\perp ^{KZ}$ is proportional to $\vert k_\| \vert / k_\perp$ (which is $\ll 1$) and since $I_\| / I_\perp \simeq 0.73$ (as checked numerically) then $\varPi _\|^{KZ} \ll \varPi _\perp ^{KZ}$, which is consistent with a turbulent cascade mainly along the perpendicular direction. In figure 3, we show the sign of the integrands of $I_\perp$ and $I_\|$ obtained from a numerical evaluation of expression (3.5) after integration over the parallel wavenumbers, and for relatively small perpendicular dimensionless wavenumbers ($<5$). We see that for $I_\perp$ the integrand is always positive, while for $I_\|$ the integrand can be either positive or negative depending on the perpendicular wavenumbers (for the largest perpendicular wavenumbers it is always positive), but, overall, the positive sign dominates in the sense that $I_\| > 0$. Therefore, the parallel cascade is also direct but it is composed of different contributions, with some triadic interactions contributing to an inverse cascade.
The energy flux being mostly perpendicular, we consider only the first line of (3.4), from which we deduce the expression of $C_E$. Then, from (2.4) we obtain (without any additional hypothesis other than $k_\perp \gg k_\parallel$)
with $C_K$ the Kolmogorov constant, which can be measured by direct numerical simulation or experimentally.
On the theoretical side, to estimate the value of $C_K$, we need to rewrite the expression of $I_\perp$. First of all, we integrate expression (3.5) over the parallel wavenumbers. Secondly, because $I_\perp$ is only defined on the domain $\varDelta _\perp$, we introduce the change of variable $\tilde {q}_\perp \equiv a-\tilde {p}_\perp$ where $1 \le a < +\infty$ and $a-1 \le 2 \tilde {p}_\perp \le a+1$ which confines the integration to this domain (see figure 2). We obtain
where
is a coefficient with the following symmetries:
which reduces by two the number of integrals to compute (four instead of eight). A numerical integration of (3.7) gives finally
In figure 4, we show the convergence of $C_K$ to this value as $a$ goes to infinity.
4. Conclusion and discussion
In this article, we first derive the locality conditions for inertial wave turbulence and verify that the anisotropic KZ spectrum – which is an exact stationary solution of the problem – satisfies these conditions. The locality of the solution ensures: (i) the finiteness of the associated flux; and (ii) the existence of an inertial range independent of large and small scales where forcing and dissipation can occur. Next, neglecting the parallel energy flux, we provide an estimate of the Kolmogorov constant that could be verified by direct numerical simulation or experimentally. Our study completes that carried out by Galtier (Reference Galtier2003) and provides theoretical support for recent numerical and experimental studies where energy spectra consistent with the prediction of inertial wave turbulence theory have been reported (Le Reun et al. Reference Le Reun, Favier and Le Bars2020; Monsalve et al. Reference Monsalve, Brunet, Gallet and Cortet2020; Yokoyama & Takaoka Reference Yokoyama and Takaoka2021).
Although the parallel energy flux is positive (like the perpendicular flux), we show numerically that it is in fact the sum of positive and negative contributions. In other words, in the parallel direction, we have triadic interactions that lead to both direct and inverse transfers, with an overall direct cascade. This observation gives some support to experimental results (Morize et al. Reference Morize, Moisy and Rabaud2005) showing that the dynamics along the axis of rotation is more difficult to identify than the transverse one, as they exhibit inverse cascade signatures. The presence of an inverse cascade in rotating turbulence is often interpreted as the interaction between the slow mode (i.e. the fluctuations at $k_\parallel = 0$) and inertial waves (Smith & Waleffe Reference Smith and Waleffe1999). However, in our case the dynamics of the slow mode is not described by the kinetic equation and the observation made is based solely on the dynamics of inertial wave turbulence.
The theory of inertial wave turbulence was originally developed for energy and helicity for which two coupled kinetic equations were derived (Galtier Reference Galtier2003). Here, helicity is neglected for several reasons. First, it simplifies the mathematical analysis and the physical interpretation. Secondly, in the presence of helicity, we cannot derive the Kolmogorov constant because it involves two terms, even if we neglect the parallel flux. Thirdly, numerical simulations are often performed initially without helicity (Bellet et al. Reference Bellet, Godeferd, Scott and Cambon2006). Some helicity may, of course, be produced, but it does not usually change the overall dynamics very much. Fourthly, the study with helicity shows that only the state of maximal helicity can give a KZ spectrum, but this situation is not natural, as the system quickly breaks this initial assumption, unless it is maintained artificially (Biferale, Musacchio & Toschi Reference Biferale, Musacchio and Toschi2012).
The locality of the KZ spectrum gives some support to the limit of super-local interactions sometimes taken to simplify the study of wave turbulence. Under this limit, a nonlinear diffusion equation is found analytically with which the numerical study becomes much easier (Galtier & David Reference Galtier and David2020). Interestingly, it was shown with this model that the non-stationary solution exhibits a $\sim k_\perp ^{-8/3}$ spectrum, which is understood as a self-similar solution of the second kind, before forming – as expected – the KZ stationary spectrum after a bounce at small scales. Note that this diffusion equation is similar to that derived in plasma physics to study solar wind turbulence (David & Galtier Reference David and Galtier2019), which opens the door to laboratory analysis of space plasmas.
Declaration of interests
The authors report no conflict of interest.