Increases of ion fluxes in the keV-MeV range are sometimes observed near the heliospheric current sheet (HCS) during periods when other sources are absent. These resemble solar energetic particle events, but the events are weaker and apparently local. Conventional explanations based on either shock acceleration of charged particles or particle acceleration due to magnetic reconnection at interplanetary current sheets (CSs) are not persuasive. We suggest instead that recurrent magnetic reconnection occurs at the HCS and smaller CSs in the solar wind, a consequence of which is particle energization by the dynamically evolving secondary CSs and magnetic islands. The effectiveness of the trapping and acceleration process associated with magnetic islands depends in part on the topology of the HCS. We show that the HCS possesses ripples superimposed on the large-scale flat or wavy structure. We conjecture that the ripples can efficiently confine plasma and provide tokamak-like conditions that are favorable for the appearance of small-scale magnetic islands that merge and/or contract. Particles trapped in the vicinity of merging islands and experiencing multiple small-scale reconnection events are accelerated by the induced electric field and experience first-order Fermi acceleration in contracting magnetic islands according to the transport theory of Zank et al. We present multi-spacecraft observations of magnetic island merging and particle energization in the absence of other sources, providing support for theory and simulations that show particle energization by reconnection related processes of magnetic island merging and contraction.
A modified method is presented to generate artificial magnetic turbulence
that is used for test-particle simulations. Such turbulent fields are obtained
from the superposition of a set of wave modes with random polarizations and
random directions of propagation. First, it is shown that the new method
simultaneously fulfils requirements of isotropy, equal mean amplitude and
variance for all field components, and vanishing divergence. Second, the number
of wave modes required for a stochastic particle behavior is investigated by
using a Lyapunov approach. For the special case of slab turbulence, it is shown
that already for 16 wave modes the particle behavior agrees with that shown for
considerably larger numbers of wave modes.Comment: 9 pages, 7 figures, accepted for publication in Phys. Plasma
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