Multi-ion oscillitons - origin of magnetospheric EMIC waves and further
implications
Abstract
The recent spacecraft observations by MMS and Van Allen Probes
associated with electromagnetic ion cyclotron waves (EMIC) in the Earth
magnetosphere emphasize the important role of multi-ion plasma
composition for generation and characteristics of these emissions. We
show that the main properties of EMIC waves can be explained with the
concept of ‘multi-ion oscillitons’ (Sauer et al., 2001). In a plasma
with two types of ions of different masses (e.g. protons and oxygen
ions), oscillitons arise from the exchange of momentum and energy
between the two ion components, with the electromagnetic field acting as
a mediator. At frequencies near cross-over frequencies of different wave
modes in the multi-ion plasma the nonlinear resonance which strongly
amplifies the seed unstable mode can be excited. A small phase
difference in oscillations of different ion species leads to a nonlinear
wave beating and generation of wave packets. The ‘resonance ‘ frequency
is characterized by a local maximum of the phase velocity and the
coincidence of phase and group velocity. The generation of coherent
waves by oscillitons is of a general nature and may contribute to
understand the manifold of phenomena in other space plasma environments
in which the dynamics of minor ion admixtures cannot be neglected, as
alpha particles in the solar wind and heavy ions around active comets.
The concept of oscillitons also applies to the momentum exchange between
different particle groups of the same mass. On this way, whistler
oscillitons may arise in two-temperature electron plasmas.