Open AccessStochastic Fermi acceleration in the magnetotail current sheet: A numerical study
Author(s) -
Greco A.,
Perri S.,
Zimbardo G.
Publication year - 2010
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009ja014690
Subject(s) - physics , fermi acceleration , electric field , acceleration , proton , magnetic field , particle acceleration , current sheet , computational physics , electromagnetic field , fermi gamma ray space telescope , atomic physics , quantum electrodynamics , magnetohydrodynamics , classical mechanics , condensed matter physics , nuclear physics , quantum mechanics
A numerical study has been carried out in order to investigate the effects of model time‐dependent electromagnetic fields along with stationary, constant electric and magnetic field components on the ion dynamics. In the Earth's magnetotail, the trajectories of thermal protons are integrated in a 2‐D model where they can experience a Fermi‐like acceleration process by interacting with synthetic oscillating electromagnetic clouds, randomly positioned within the xy plane. Besides the time‐dependent fluctuations, a dawn‐dusk electric field component E 0 y is present, as well as a constant out‐of‐plane magnetic field component B n . When the size of the electromagnetic clouds is small compared to the simulation box sides, the proton acceleration is mostly due to the dawn‐dusk electric field; increasing B n causes a reduction of the obtained energies, reduction which decreases when B n is further increased. For larger sizes of the electromagnetic blobs, Fermi acceleration becomes more efficient, and proton energies up to 100 keV are obtained. In such a case, the influence of the constant fields E 0 y and B n becomes weak, and the final energy distribution does not depend on B n . This means that the stochastic Fermi acceleration can be efficient even in the presence of a background magnetic field. Since the typical energies of protons are in good agreement with those observed for proton beams in the Earth's magnetotail, the joint effects of the random fields and the steady ones can explain particle acceleration processes in the distant and the near‐Earth magnetotail regions.