Effect of interchange instability on magnetic reconnection

We present here the results of a study of interacting magnetic fields that involves a force normal to the reconnection layer. In the presence of such force, the reconnection layer becomes unstable to interchange disturbances. The interchange instability results in formation of tongues of heated plas...

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Main Authors: W. Lyatsky, M. L. Goldstein
Format: Article
Language:English
Published: Copernicus Publications 2013-06-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/20/365/2013/npg-20-365-2013.pdf
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spelling doaj-a2d3295443124fc4a6eec195db8b58a32020-11-25T01:36:03ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462013-06-0120336537710.5194/npg-20-365-2013Effect of interchange instability on magnetic reconnectionW. LyatskyM. L. GoldsteinWe present here the results of a study of interacting magnetic fields that involves a force normal to the reconnection layer. In the presence of such force, the reconnection layer becomes unstable to interchange disturbances. The interchange instability results in formation of tongues of heated plasma that leaves the reconnection layer through its wide surface rather than through its narrow ends, as is the case in traditional magnetic reconnection models. This plasma flow out of the reconnection layer facilitates the removal of plasma from the layer and leads to fast reconnection. The proposed mechanism provides fast reconnection of interacting magnetic fields and does not depend on the thickness of the reconnection layer. This instability explains the strong turbulence and bidirectional streaming of plasma that is directed toward and away from the reconnection layer that is observed frequently above reconnection layers. The force normal to the reconnection layer also accelerates the removal of plasma islands appearing in the reconnection layer during turbulent reconnection. In the presence of this force normal to the reconnection layer, these islands are removed from the reconnection layer by the "buoyancy force", as happens in the case of interchange instability that arises due to the polarization electric field generated at the boundaries of the islands.http://www.nonlin-processes-geophys.net/20/365/2013/npg-20-365-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author W. Lyatsky
M. L. Goldstein
spellingShingle W. Lyatsky
M. L. Goldstein
Effect of interchange instability on magnetic reconnection
Nonlinear Processes in Geophysics
author_facet W. Lyatsky
M. L. Goldstein
author_sort W. Lyatsky
title Effect of interchange instability on magnetic reconnection
title_short Effect of interchange instability on magnetic reconnection
title_full Effect of interchange instability on magnetic reconnection
title_fullStr Effect of interchange instability on magnetic reconnection
title_full_unstemmed Effect of interchange instability on magnetic reconnection
title_sort effect of interchange instability on magnetic reconnection
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2013-06-01
description We present here the results of a study of interacting magnetic fields that involves a force normal to the reconnection layer. In the presence of such force, the reconnection layer becomes unstable to interchange disturbances. The interchange instability results in formation of tongues of heated plasma that leaves the reconnection layer through its wide surface rather than through its narrow ends, as is the case in traditional magnetic reconnection models. This plasma flow out of the reconnection layer facilitates the removal of plasma from the layer and leads to fast reconnection. The proposed mechanism provides fast reconnection of interacting magnetic fields and does not depend on the thickness of the reconnection layer. This instability explains the strong turbulence and bidirectional streaming of plasma that is directed toward and away from the reconnection layer that is observed frequently above reconnection layers. The force normal to the reconnection layer also accelerates the removal of plasma islands appearing in the reconnection layer during turbulent reconnection. In the presence of this force normal to the reconnection layer, these islands are removed from the reconnection layer by the "buoyancy force", as happens in the case of interchange instability that arises due to the polarization electric field generated at the boundaries of the islands.
url http://www.nonlin-processes-geophys.net/20/365/2013/npg-20-365-2013.pdf
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