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Long-term evolution of electron distribution function due to nonlinear resonant interaction with whistler mode waves

Published online by Cambridge University Press:  05 April 2018

Anton V. Artemyev*
Affiliation:
Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California, USA Space Research Institute, Moscow, Russia
Anatoly I. Neishtadt
Affiliation:
Space Research Institute, Moscow, Russia Department of Mathematical Sciences, Loughborough University, Loughborough LE11 3TU, UK
Alexei A. Vasiliev
Affiliation:
Space Research Institute, Moscow, Russia
Didier Mourenas
Affiliation:
CEA, DAM, DIF, Arpajon, France
*
†Email address for correspondence: aartemyev@igpp.ucla.edu
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Abstract

Accurately modelling and forecasting of the dynamics of the Earth’s radiation belts with the available computer resources represents an important challenge that still requires significant advances in the theoretical plasma physics field of wave–particle resonant interaction. Energetic electron acceleration or scattering into the Earth’s atmosphere are essentially controlled by their resonances with electromagnetic whistler mode waves. The quasi-linear diffusion equation describes well this resonant interaction for low intensity waves. During the last decade, however, spacecraft observations in the radiation belts have revealed a large number of whistler mode waves with sufficiently high intensity to interact with electrons in the nonlinear regime. A kinetic equation including such nonlinear wave–particle interactions and describing the long-term evolution of the electron distribution is the focus of the present paper. Using the Hamiltonian theory of resonant phenomena, we describe individual electron resonance with an intense coherent whistler mode wave. The derived characteristics of such a resonance are incorporated into a generalized kinetic equation which includes non-local transport in energy space. This transport is produced by resonant electron trapping and nonlinear acceleration. We describe the methods allowing the construction of nonlinear resonant terms in the kinetic equation and discuss possible applications of this equation.

Information

Type
Research Article
Copyright
© Cambridge University Press 2018 
Figure 0

Figure 1. Scheme of particle energy $\unicode[STIX]{x1D6FE}$ change over a time $T$ due to diffusion and due to non-local transport.

Figure 1

Figure 2. Functions $C_{1}$, $C_{2}$ given by (2.3), and functions $C=\sqrt{C_{1}C_{2}}$, $C_{3}=(N^{2}\unicode[STIX]{x1D700}_{3}^{-1}-1)/$$N\cos \unicode[STIX]{x1D703}$ for $\unicode[STIX]{x1D714}/\unicode[STIX]{x1D6FA}_{0}=0.35$ and $\unicode[STIX]{x1D6FA}_{\text{pe}}/\unicode[STIX]{x1D6FA}_{0}=4.5$ at $\unicode[STIX]{x1D706}=0$, considering field-aligned ($\unicode[STIX]{x1D703}=0$) and highly oblique waves near the resonance cone angle $\unicode[STIX]{x1D703}_{r}$.

Figure 2

Figure 3. Normalized area $S_{\text{sep}}(\unicode[STIX]{x1D6FE})$ given by (2.27).

Figure 3

Figure 4. (a) Refractive index $N_{\Vert }$, derivative $\unicode[STIX]{x2202}\ln \unicode[STIX]{x1D6FA}_{0}/\unicode[STIX]{x2202}s/R$ and field-aligned coordinate $s$ are shown as functions of $\unicode[STIX]{x1D706}$. (b) System parameter $\unicode[STIX]{x1D700}_{0}$ as a function of initial energy and pitch angle. (c) Periods $T(\unicode[STIX]{x1D6FE})$ and resonant latitudes are shown for three values of $\unicode[STIX]{x1D700}_{0}$ in the case of parallel whistler mode waves.

Figure 4

Figure 5. Functions $\bar{r}(\unicode[STIX]{x1D6FE})$ (a), $\langle \unicode[STIX]{x0394}\unicode[STIX]{x1D6FE}\rangle (\unicode[STIX]{x1D6FE})$ (b), $J(\unicode[STIX]{x1D6FE})$ (c) are shown for three values of $\unicode[STIX]{x1D700}_{0}$ in the case of parallel whistler mode waves.

Figure 5

Figure 6. The case of parallel whistler mode waves. Dependencies $\unicode[STIX]{x1D6FE}=Y(\unicode[STIX]{x1D6FE}^{\ast })$ for three $\unicode[STIX]{x1D700}_{0}$ values: $\unicode[STIX]{x1D700}_{0}=-3$ (a), $\unicode[STIX]{x1D700}_{0}=-4$ (b), $\unicode[STIX]{x1D700}_{0}=-6$ (c).

Figure 6

Figure 7. The case of parallel whistler mode waves. (a,c,e) Show the distributions of $\unicode[STIX]{x1D702}^{-1/2}V_{J}(J)$, $-\unicode[STIX]{x1D702}^{-1/2}\,\text{d}V_{J}/\text{d}J$, and $J^{\ast }(J)$ (inverse $Y_{J}(J^{\ast })$ function). (b,d,f) Show the distributions $\unicode[STIX]{x1D6F9}_{J}(J)$ (dashed) and $\unicode[STIX]{x1D6F9}(\unicode[STIX]{x1D6FE})$ (solid) at three different times $tc/R$. The data are plotted for three different $\unicode[STIX]{x1D700}_{0}$ values.

Figure 7

Figure 8. The case of very oblique whistler mode waves. (a) Refractive index $N_{\Vert }$ and $\cos \unicode[STIX]{x1D703}$ are shown as functions of $\unicode[STIX]{x1D706}$. (b) System parameter $\unicode[STIX]{x1D700}_{0}$ as a function of initial energy and pitch angle. (c) Periods $T(\unicode[STIX]{x1D6FE})$ and resonant latitudes for three values of $\unicode[STIX]{x1D700}_{0}$.

Figure 8

Figure 9. Functions $\bar{r}(\unicode[STIX]{x1D6FE})$ (a), $\langle \unicode[STIX]{x0394}\unicode[STIX]{x1D6FE}\rangle (\unicode[STIX]{x1D6FE})$ (b), $J(\unicode[STIX]{x1D6FE})$ (c) for three different values of $\unicode[STIX]{x1D700}_{0}$ in the case of very oblique whistler mode waves.

Figure 9

Figure 10. Dependencies $\unicode[STIX]{x1D6FE}=Y(\unicode[STIX]{x1D6FE}^{\ast })$ for three $\unicode[STIX]{x1D700}_{0}$ values in the case of very oblique whistler mode waves: $\unicode[STIX]{x1D700}_{0}=0.5$ (a), $\unicode[STIX]{x1D700}_{0}=1$ (b), $\unicode[STIX]{x1D700}_{0}=2$ (c).

Figure 10

Figure 11. (a,c,e) Show distributions of $\unicode[STIX]{x1D702}^{-1/2}V_{J}(J)$, $-\unicode[STIX]{x1D702}^{-1/2}\,\text{d}V_{J}/\text{d}J$ and $J^{\ast }(J)$ (inverse $Y_{J}(J^{\ast })$ function). (b,d,f) Show the distributions $\unicode[STIX]{x1D6F9}_{J}(J)$ (dashed) and $\unicode[STIX]{x1D6F9}(\unicode[STIX]{x1D6FE})$ (solid) at three different times $tc/R$. Data are plotted for three $\unicode[STIX]{x1D700}_{0}$ values in the case of highly oblique whistler mode waves.