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Imbalanced kinetic Alfvén wave turbulence: from weak turbulence theory to nonlinear diffusion models for the strong regime

Published online by Cambridge University Press:  16 May 2019

T. Passot*
Affiliation:
Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire J.L. Lagrange, Boulevard de l’Observatoire, CS 34229, 06304 Nice CEDEX 4, France
P. L. Sulem
Affiliation:
Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire J.L. Lagrange, Boulevard de l’Observatoire, CS 34229, 06304 Nice CEDEX 4, France
*
†Email address for correspondence: passot@oca.eu
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Abstract

A two-field Hamiltonian gyrofluid model for kinetic Alfvén waves retaining ion finite Larmor radius corrections, parallel magnetic field fluctuations and electron inertia, is used to study turbulent cascades from the magnetohydrodynamic (MHD) to the sub-ion scales. Special attention is paid to the case of imbalance between waves propagating along or opposite to the ambient magnetic field. For weak turbulence in the absence of electron inertia, kinetic equations for the spectral density of the conserved quantities (total energy and generalized cross-helicity) are obtained. They provide a global description, matching between the regimes of reduced MHD at large scales and electron reduced MHD at small scales, previously considered in the literature. In the limit of ultra-local interactions, Leith-type nonlinear diffusion equations in the Fourier space are derived and heuristically extended to the strong turbulence regime by modifying the transfer time appropriately. Relations with existing phenomenological models for imbalanced MHD and balanced sub-ion turbulence are discussed. It turns out that in the presence of dispersive effects, the dynamics is sensitive on the way turbulence is maintained in a steady state. Furthermore, the total energy spectrum at sub-ion scales becomes steeper as the generalized cross-helicity flux is increased.

Information

Type
Research Article
Copyright
© Cambridge University Press 2019 
Figure 0

Table 1. Asymptotic forms of the Fourier symbols (indicated by a caret) of the operators $M_{1}$, $M_{2}$, $\unicode[STIX]{x1D6EC}$ and $V_{ph}$, together with the corresponding equation numbers, in four different regimes.

Figure 1

Figure 1. (a) Spectra $E(k_{\bot })$ (red) and $|E_{C}(k_{\bot })|$ (green); (b) spectra $E^{+}(k_{\bot })$ (red) and $E^{-}(k_{\bot })$ (green); (c) slopes $m^{+}(k_{\bot })$ (red), $m^{-}(k_{\bot })$ (green) and $m^{+}+m^{-}$ (blue). The simulation was performed with $\unicode[STIX]{x1D6FD}_{e}=2$, $\unicode[STIX]{x1D70F}=1$ in the weak turbulence regime in the case of a weak transfer rate of generalized cross-helicity $\unicode[STIX]{x1D702}/\unicode[STIX]{x1D700}=0.008$, but a relatively large value of $k_{d}=120$. Other parameters are $\widetilde{k}_{\Vert }^{\pm }=1$, $C^{\prime }=1$, $\unicode[STIX]{x1D700}=1$, $u^{+}(k_{d})=u^{-}(k_{d})=(1/2)(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$.

Figure 2

Figure 2. Same as figure 1, but for $\unicode[STIX]{x1D702}/\unicode[STIX]{x1D700}=0.05$ and $k_{d}=15$.

Figure 3

Figure 3. $E^{+}$ (red) and $E^{-}$ (green) spectra (a–c) together with the local slopes (bottom) $m^{+}$ (red), $m^{-}$ (green) and $m^{+}+2m^{-}$ (blue) in the strong turbulence regime, for $\unicode[STIX]{x1D708}=0$ (a,d), $\unicode[STIX]{x1D708}=0.8$ (b,e) and $\unicode[STIX]{x1D708}=1$ (c,f). The other parameters are $\unicode[STIX]{x1D700}=1$, $k_{f}=0$, $k_{d}=100$ with $u^{+}(k_{d})=u^{-}(k_{d})=50(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$. The values $\unicode[STIX]{x1D702}=0.93869$ for $\unicode[STIX]{x1D708}=0$, $\unicode[STIX]{x1D702}=0.33477$ for $\unicode[STIX]{x1D708}=0.8$ and $\unicode[STIX]{x1D702}=0.07115$ for $\unicode[STIX]{x1D708}=1$ are chosen such that $E^{+}(10^{-6})/E^{-}(10^{-6})\approx 1000$ in all the cases.

Figure 4

Figure 4. $E^{+}$ (red) and $E^{-}$ (green) spectra in the strong turbulence regime. (a) For $\unicode[STIX]{x1D708}=1$, $\unicode[STIX]{x1D700}=1$, $\unicode[STIX]{x1D702}=0.01$, $k_{d}=200$, $k_{f}=0$ with $u^{+}(k_{d})=u^{-}(k_{d})=0.23552\;(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$; (b) for $\unicode[STIX]{x1D708}=0$, $\unicode[STIX]{x1D700}=0.1$, $k_{f}=0.5$, $k_{d}=60$ with $u^{+}(k_{d})=u^{-}(k_{d})=(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$, $\unicode[STIX]{x1D702}=0.053752\unicode[STIX]{x1D700}$ (singular point $E^{-}=0$ at $k_{\ast }\approx 23$); (c) case $k_{\ast }>k_{d}$ for $\unicode[STIX]{x1D708}=0$, $\unicode[STIX]{x1D700}=0.1$, $\unicode[STIX]{x1D702}=0.015$ (giving $k_{\ast }\approx 82$) $k_{f}=0.5$, $k_{d}=60$ when choosing the critical value $u^{+}(k_{d})=u^{-}(k_{d})=u_{c}\equiv 0.405176\;(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$ for which $E^{+}$ decays but $E^{-}$ tends to the absolute equilibrium.

Figure 5

Figure 5. A case with $\unicode[STIX]{x1D708}=1$, $\unicode[STIX]{x1D700}=1$, $\unicode[STIX]{x1D702}/\unicode[STIX]{x1D700}=0.005$, $k_{d}=500$, $u^{+}(k_{d})=u^{-}(k_{d})=10^{3}(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$, $k_{f}=0$. In (a,b) are shown the $E^{\pm }$ spectra (a,c), and $\widetilde{k}_{\Vert }^{\pm }$ (b,d), while in (c,d) are displayed the local slopes $m^{\pm }(k_{\bot })$ together with $m^{+}+2m^{-}$ (in blue) (a,c) and the nonlinearity parameters $\unicode[STIX]{x1D712}^{\pm }=(k_{\bot }^{3}E^{\pm }(k_{\bot }))^{1/2}/\widetilde{k}_{\Vert }^{\pm }$ (b,d). In all these graphs, red (green) colour refers to $+$ ($-$) waves.

Figure 6

Figure 6. A case with $\unicode[STIX]{x1D708}=1$, $\unicode[STIX]{x1D700}=1$, $\unicode[STIX]{x1D702}/\unicode[STIX]{x1D700}=0.045$, $k_{d}=200$, $u^{+}(k_{d})=u^{-}(k_{d})=2\times 10^{3}(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$, $k_{f}=5\times 10^{-3}$ where the $-$ component remains in the weak turbulence regime, while the $+$ one undergoes a transition to strong turbulence. In the top panels are shown the $E^{\pm }$ spectra (a,c), and $\widetilde{k}_{\Vert }^{\pm }$ (b,d), while in the bottom panels are displayed the local slopes $m^{\pm }(k_{\bot })$ together with $m^{+}+2m^{-}$ (in blue) (a,c) and the nonlinearity parameters $\unicode[STIX]{x1D712}^{\pm }=(k_{\bot }^{3}E^{\pm }(k_{\bot }))^{1/2}/\widetilde{k}_{\Vert }^{\pm }$ (b,d). In all these graphs, red (green) colour refers to $+$ ($-$) waves.

Figure 7

Figure 7. (a) Total energy spectra obtained for $\unicode[STIX]{x1D702}=0$ (red), $\unicode[STIX]{x1D702}=2\times 10^{-3}$ (green), $\unicode[STIX]{x1D702}=5\times 10^{-3}$ (blue), $\unicode[STIX]{x1D702}=8\times 10^{-3}$ (black) and $\unicode[STIX]{x1D702}=9\times 10^{-3}$ (violet), with $\unicode[STIX]{x1D700}=1$, $k_{d}=200$, $k_{f}=0$, $u^{+}(k_{d})=u^{-}(k_{d})=0.6(\unicode[STIX]{x1D700}/k_{d}^{7})^{1/2}$; (b) normalized cross-helicity spectrum $E_{C}(k_{\bot })/E(k_{\bot })$ for $\unicode[STIX]{x1D702}=2\times 10^{-3}$ and $\unicode[STIX]{x1D702}=9\times 10^{-3}$, the other parameters being the same as in (b).