On a transitional regime of electron resonant interaction with whistler-mode waves in inhomogeneous space plasma

TL;DR

This paper develops a theoretical framework to quantify the transition between diffusive and nonlinear resonant interactions of electrons with whistler-mode waves in space plasma, enhancing understanding of energetic electron dynamics.

Contribution

It introduces a model for the nonlinear interaction rate D(NL) and compares it with the quasi-linear rate D(QL), defining the conditions where both regimes are equally effective.

Findings

Derived the scaling of D(NL) with wave intensity and wave-packet size.

Identified the wave conditions where diffusive and nonlinear regimes have similar electron evolution rates.

Discussed implications for energetic electron behavior in Earth's radiation belt.

Abstract

Resonances with electromagnetic whistler-mode waves are the primary driver for the formation and dynamics of energetic electron fluxes in various space plasma systems, including shock waves and planetary radiation belts. The basic and most elaborated theoretical framework for the description of the integral effect of multiple resonant interactions is the quasi-linear theory, that operates through electron diffusion in velocity space. The quasi-linear diffusion rate scales linearly with the wave intensity, D(QL) is proportional to Bw2, which should be small enough to satisfy the applicability criteria of this theory. Spacecraft measurements, however, often detect whistle-mode waves sufficiently intense to resonate with electrons nonlinearly. Such nonlinear resonant interactions imply effects of phase trapping and phase bunching, which may quickly change the electron fluxes in a non-diffusive manner. Both regimes of electron resonant interactions (diffusive and nonlinear) are well studied, but there is no theory quantifying the transition between these two regimes. In this paper we describe the integral effect of nonlinear electron interactions with whistler-mode waves in terms of the time-scale of electron distribution relaxation, is about inverse D(NL). We determine the scaling of D(NL) with wave intensity Bw2 and other main wave characteristics, such as wave-packet size. The comparison of D(QL) and D(NL) provides the range of wave intensity and wave-packet sizes where the electron distribution evolves at the same rates for the diffusive and nonlinear resonant regimes. The obtained results are discussed in the context of energetic electron dynamics in the Earth's radiation belt.