Abstract
Abstract. We report on the nonlinear turbulent processes associated with electromagnetic waves in plasmas. We focus on low-frequency (in comparison with the electron gyrofrequency) nonlinearly interacting electron whistlers and nonlinearly interacting Hall-magnetohydrodynamic (H-MHD) fluctuations in a magnetized plasma. Nonlinear whistler mode turbulence study in a magnetized plasma involves incompressible electrons and immobile ions. Two-dimensional turbulent interactions and subsequent energy cascades are critically influenced by the electron whisters that behave distinctly for scales smaller and larger than the electron skin depth. It is found that in whistler mode turbulence there results a dual cascade primarily due to the forward spectral migration of energy that coexists with a backward spectral transfer of mean squared magnetic potential. Finally, inclusion of the ion dynamics, resulting from a two fluid description of the H-MHD plasma, leads to several interesting results that are typically observed in the solar wind plasma. Particularly in the solar wind, the high-time-resolution databases identify a spectral break at the end of the MHD inertial range spectrum that corresponds to a high-frequency regime. In the latter, turbulent cascades cannot be explained by the usual MHD model and a finite frequency effect (in comparison with the ion gyrofrequency) arising from the ion inertia is essentially included to discern the dynamics of the smaller length scales (in comparison with the ion skin depth). This leads to a nonlinear H-MHD model, which is presented in this paper. With the help of our 3-D H-MHD code, we find that the characteristic turbulent interactions in the high-frequency regime evolve typically on kinetic-Alfvén time-scales. The turbulent fluctuation associated with kinetic-Alfvén interactions are compressive and anisotropic and possess equipartition of the kinetic and magnetic energies.
Highlights
Many laboratory and space plasmas contain multi-scale electromagnetic fluctuations
While the wavelengths of the electron whistlers could be comparable with the electron skin depth, the HMHD fluctuations could have differential wavelengths when compared with the ion skin depth and the ion-sound gyroradius
The electron whistlers are described by the electron magnetohydrodynamics (EMHD) equations (Kingsep et al, 1990), and the role of whistlers in the EMHD turbulence is an unresolved issue (Shaikh et al, 2000a,b; Shaikh, 2004, 2008, 2009; Shaikh and Zank, 2003, 2005)
Summary
Many laboratory and space plasmas contain multi-scale electromagnetic fluctuations. The latter include the electron whistlers and H-MHD fluctuations in a uniform magnetoplasma. One can have different types of electromagnetic waves The latter include the low-frequency (in comparison with the electron gyrofrequency) electron whistlers as well as linearly coupled fast and slow magnetosonic and kinetic-Alfven waves. Numerical simulations of inverse cascade phenomenon, within the context of magnetohydrodynamics (MHD) turbulence, have previously been performed at a modest resolution of up to 10242 Fourier modes (Biskamp and Bremer, 1994).
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