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Diffusive scattering of energetic electrons by intense whistler-mode waves in an inhomogeneous plasma

Published online by Cambridge University Press:  06 January 2023

Viktor A. Frantsuzov*
Affiliation:
Space Research Institute of the Russian Academy of Sciences (IKI), 84/32 Profsoyuznaya Str., Moscow 117997, Russia Faculty of Physics, National Research University Higher School of Economics, 21/4 Staraya Basmannaya Ulitsa, Moscow 105066, Russia
Anton V. Artemyev
Affiliation:
Space Research Institute of the Russian Academy of Sciences (IKI), 84/32 Profsoyuznaya Str., Moscow 117997, Russia Institute of Geophysics and Planetary Physics, UCLA, Los Angeles, CA 90095, USA
Xiao-Jia Zhang
Affiliation:
Institute of Geophysics and Planetary Physics, UCLA, Los Angeles, CA 90095, USA
Oliver Allanson
Affiliation:
Department of Mathematics, University of Exeter, Penryn/Cornwall Campus, Penryn, TR10 9FE, UK
Pavel I. Shustov
Affiliation:
Space Research Institute of the Russian Academy of Sciences (IKI), 84/32 Profsoyuznaya Str., Moscow 117997, Russia Faculty of Physics, National Research University Higher School of Economics, 21/4 Staraya Basmannaya Ulitsa, Moscow 105066, Russia
Anatoli A. Petrukovich
Affiliation:
Space Research Institute of the Russian Academy of Sciences (IKI), 84/32 Profsoyuznaya Str., Moscow 117997, Russia
*
†Email address for correspondence: vafrantsuzov@outlook.com
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Abstract

Electron resonant interactions with electromagnetic whistler-mode waves play an important role in electron flux dynamics in various space plasma systems: planetary radiation belts, bow shocks, solar wind and magnetic reconnection regions. Two key wave characteristics determining the regime of wave–particle interactions are the wave intensity and the wave coherency. The classical quasi-linear diffusion approach describes well electron diffusion by incoherent and low-amplitude waves, whereas the nonlinear resonant models describe electron phase bunching and trapping by highly coherent intense waves. This study is devoted to the investigation of the regime of electron resonant interactions with incoherent but intense waves. Although this regime is characterized by electron diffusion, we show that diffusion rates scale linearly with the wave amplitude, $D\propto B_w$, in contrast to the quasi-linear diffusion scaling $D_{QL}\propto B_w^2$. Using observed wave amplitude distributions, we demonstrate that the quasi-linear diffusion model significantly overestimates electron scattering by incoherent, but intense whistler-mode waves. We discuss the results obtained in the context of simulations of long-term electron flux dynamics in space plasma systems.

Information

Type
Research Article
Copyright
Copyright © The Author(s), 2023. Published by Cambridge University Press
Figure 0

Figure 1. Examples of typical wave packets of whistler-mode waves captured by THEMIS spacecraft (Angelopoulos 2008) in the Earth bow shock (a), foreshock transient (b), outer radiation belt (c) and plasma injection region (d). These events are picked up from statistics published in Artemyev et al. (2022), Shi et al. (2020), Zhang et al. (2018b) and Zhang et al. (2018a).

Figure 1

Figure 2. A set of trajectories obtained by the numerical integration of Hamiltonian equations for a system (2.10a,b). Results are shown for (a) low-amplitude wave with diffusive scattering, (b) coherent high-amplitude wave with trapping and bunching and (c) modulated high-amplitude wave with diffusive-like scattering. System parameters are: electron energy $E_0=100$ keV, equatorial pitch angle $\alpha _0 = 40^\circ$, number of particles $N = 100$, wave amplitude $B_w = 5$ pT (a), $B_w = 500$ pT (b,c). System parameters correspond to $L\text {-shell} = 6$, whistler-mode waves with frequency equal to $0.35$ of the electron cyclotron frequency at the equator, and the constant plasma frequency equal to $10$ times the electron cyclotron frequency at the equator.

Figure 2

Figure 3. Distributions of the energy change $\Delta E$ for different $B_{{\rm eff}}$ with $h=1$ and $l=20$ for coherent (a–c) and modulated (d–f) waves with $\Delta E \propto B_w$ fitting (black dashed lines) and with $\langle {(\Delta E)^2}\rangle ^{1/2}$ profiles (black dots): (a,d) $E_0 = 100$ keV, $\alpha _0 = 40^{\circ }$; (b,e) $E_0 = 100$ keV, $\alpha _0 = 60^{\circ }$; (c, f) $E_0 = 300$ keV, $\alpha _0 = 60^{\circ }$. For each $B_w$ we use $10^4$ trajectories to evaluate the $\Delta E$ distribution, each particle resonates with the wave only once and $\Delta E$ is the energy change for a single resonance, initial particle phases and wave phases are random and thus for a modulated case the actual wave amplitude is different for different particles having the same energy/pitch angle. For each $B_{{\rm eff}}$ the $\Delta E$ distribution is normalized to one. System parameters correspond to $L\text {-shell} = 6$, whistler-mode waves with frequency equal to $0.35$ of the electron cyclotron frequency at the equator, and the constant plasma frequency equal to $10$ times the electron cyclotron frequency at the equator.

Figure 3

Figure 4. (a) Profiles of $f(a,\xi )$ for three $a$ values. (b) Profiles of $\langle f(a,\xi )\rangle _{\xi }$ and $\langle (f(a,\xi ))^2\rangle _{\xi }$.

Figure 4

Figure 5. Probability distributions of $\xi$ for $10^5$ trajectories and (a) $E_0 = 100$ keV, $\alpha _0 = 40^{\circ }$, $B_w = 50$ pT, (b) $E_0 = 100$ keV, $\alpha _0 = 40^{\circ }$, $B_w = 500$ pT, (c) $E_0 = 300$ keV, $\alpha _0 = 60^{\circ }$, $B_w = 500$ pT.

Figure 5

Figure 6. Two-dimensional energy/pitch-angle maps of $(E_0,\alpha _{0})$ for (a) $B_w = 100$ pT, (b) $B_w = 500$ pT and (c) $B_w = 1000$ pT. Black curve shows $a=1$.

Figure 6

Figure 7. (a) Probability distribution functions ${\mathcal {F}}(B_w/B_0)$ of whistler-mode wave intensities from Zhang et al. (2019) (blue) and Zhang et al. (2020b) (red). (b,c) Two-dimensional distributions of $\langle \langle (\Delta \gamma )^2\rangle _{\xi }/\langle (\Delta \gamma )^2\rangle _{\xi }^{QL} \rangle _{\varepsilon }$ in $(E_0,\alpha _{0})$ space for the two ${\mathcal {F}}(B_w/B_0)$ distributions from (a).

Figure 7

Figure 8. A schematic view of diffusion rate scaling with wave amplitude normalized to the amplitude threshold for nonlinear resonant interactions, $B_w^{*}$. Quasi-linear diffusion rate $D_{QL}\propto B_w^2$ works only for $B_w/B_w^{*}<1$. For $B_w/B_w^{*}>1$ and incoherent waves should work $D\propto B_w$, whereas for coherent waves should work $D_{NL}\propto \sqrt {B_w}$ (see Artemyev et al.2021a).

Figure 8

Figure 9. Comparison between $\langle f^2(a,\xi ) \rangle _{\xi }$ and $\langle f(a,\xi ) \rangle _{\xi }^2$ as functions of $a$.