Physics
Scientific paper
Dec 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004agufmsm41a1127k&link_type=abstract
American Geophysical Union, Fall Meeting 2004, abstract #SM41A-1127
Physics
7807 Charged Particle Motion And Acceleration, 7843 Numerical Simulation Studies, 7867 Wave/Particle Interactions, 2720 Energetic Particles, Trapped, 2730 Magnetosphere: Inner
Scientific paper
The resonant scattering process via whistler mode waves has been recognized as the strong candidate mechanism for the acceleration process of relativistic electrons during the recovery phase of a geomagnetic storm in the inner magnetosphere. We study resonant interaction between relativistic electrons and monochromatic whistler mode waves by using a self-consistent simulation model. The simulation model is based on the model which treats background cold electrons as a fluid and hot electrons as particles by PIC method including fully relativistic effect. In the simulation system, oppositely traveling monochromatic whistler mode waves are excited by an instability associated with a temperature anisotropy of keV energy electrons. The simulation result shows that the energy transfer process takes place between relativistic electrons and keV electrons and that the monochromatic whistler mode wave traps relativistic electrons which satisfy the resonance condition. Especially, in a case that oppositely propagating monochromatic waves coexist, a combined effect of wave trapping connects diffusion curves and opens a route for the rapid acceleration. The motion of the trapped relativistic electrons in the momentum space is estimated from the intersection of resonance curves and the scale of trapping region which is determined by both trapping velocity and resonance velocity. The present simulation reveals that selected resonant electrons are effectively accelerated in a homogeneous system where both forward and backward traveling waves interact with the relativistic electrons.
Katoh Yuto
Omura Yuji
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