Frequency bands and gaps of magnetospheric chorus waves generated by
resonant beam/plateau electrons
Abstract
In this paper, the modifications of the whistler dispersion
characteristics are investigated which arise if resonant electrons are
taken into account. The following chain of processes is emphasized:
Generation of whistler waves propagating at different angles to the
magnetic field and their nonlinear interaction with resonant electrons
result in the appearance of modulated electron beams in the background
plasma. As a result, the dispersion characteristics of waves in this new
plasma might be significantly changed. By solving the kinetic dispersion
relation of whistler waves in electron plasmas with so-called
beam/plateau (b/p) populations, the associated modifications of the
whistler dispersion characteristics are presented in diagrams showing,
in particular, the frequency versus propagation angle dependence of the
excited waves. It is important to point out the two functions of the b/p
populations. The interaction of the beam-shifted cyclotron mode ω =
Ωe + k·Vb
(Vb<0, Vb is the b/p velocity,
Ωe: electron cyclotron frequency)) with the whistler
mode leads to enhanced damping at the ω-k point where they intersect.
This is the origin of the frequency gap at half the electron cyclotron
frequency (ω~Ωe/2) for quasi-parallel
waves which are driven by temperature anisotropy. Furthermore, it is
shown that the upstream b/p electrons alone (in the absence of
temperature anisotropy) can excite (very) oblique whistler waves near
the resonance cone. The governing instability results from the
interaction of the beam/plateau mode ω=k·Vb
(Vb>0) with the whistler mode. Relations to
recent and former space observations are discussed.