Journal of Geophysical Research Space Physics · 2014 · 27 citations · 43 references
Natural SciencesPhysicsElectromagneticsElectromagnetismPlasma PhysicsMagnetic DomainsMagnetohydrodynamicsCurrent Sheet DynamicsMagnetic Field LinesMagnetic Reconnection In Fusion PlasmasMagnetic Reconnection In Gamma-ray FlaresQuadrupole DeformationQuadrupole InteractionQuadrupole ModesQuadrupole Splitting
Abstract A magnetic island plays an important role in magnetic reconnection. In this paper, using a series of two‐dimensional particle‐in‐cell simulations, we investigate the magnetic structures of a magnetic island formed during multiple X line magnetic reconnections, considering the effects of the guide field in symmetric and asymmetric current sheets. In a symmetric current sheet, the current in the x direction forms a tripolar structure inside a magnetic island during antiparallel reconnection, which results in a quadrupole structure of the out‐of‐plane magnetic field. With the increase of the guide field, the symmetry of both the current system and out‐of‐plane magnetic field inside the magnetic island is distorted. When the guide field is sufficiently strong, the current forms a ring along the magnetic field lines inside a magnetic island. At the same time, the current carried by the energetic electrons accelerated in the vicinity of the X lines forms another ring at the edge of the magnetic island. Such a dual‐ring current system enhances the out‐of‐plane magnetic field inside the magnetic island with a dip in the center of the magnetic island. In an asymmetric current sheet, when there is no guide field, electrons flow toward the X lines along the separatrices from the side with a higher density and are then directed away from the X lines along the separatrices to the side with a lower density. The formed current results in the enhancement of the out‐of‐plane magnetic field at one end of the magnetic island and the attenuation at the other end. With the increase of the guide field, the structures of both the current system and the out‐of‐plane magnetic field are distorted.
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