The Alfvén edge in asymmetric reconnection

We show that in the case of magnetic reconnection where the Alfvén velocity is much higher in the plasma on one side of the current sheet than the other, an Alfvén edge is formed. This edge is located between the electron and ion edges on the high Alfvén velocity side of the current sheet. The A...

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Main Authors: A. Vaivads, A. Retinò, Yu. V. Khotyaintsev, M. André
Format: Article
Language:English
Published: Copernicus Publications 2010-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/28/1327/2010/angeo-28-1327-2010.pdf
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author A. Vaivads
A. Retinò
Yu. V. Khotyaintsev
M. André
author_facet A. Vaivads
A. Retinò
Yu. V. Khotyaintsev
M. André
author_sort A. Vaivads
collection DOAJ
description We show that in the case of magnetic reconnection where the Alfvén velocity is much higher in the plasma on one side of the current sheet than the other, an Alfvén edge is formed. This edge is located between the electron and ion edges on the high Alfvén velocity side of the current sheet. The Alfvén edge forms because the Alfvén wave generated near the X-line will propagate faster than the accelerated ions forming the ion edge. We discuss possible generation mechanism and the polarization of the Alfvén wave in the case when higher Alfvén speed is due to larger magnetic field and smaller plasma density, as in the case of magnetopause reconnection. The Alfvén wave can be generated due to Hall dynamics near the X-line. The Alfvén wave pulse has a unipolar electric field and the parallel current will be such that the outer current on the high magnetic field side is flowing away from the X-line. Understanding Alfvén edges is important for understanding the separatrix regions at the boundaries of reconnection jets. We present an example of Alfvén edge observed by the Cluster spacecraft at the magnetopause.
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spelling doaj.art-ddd5195fe49e4c50a85708196832aa292022-12-21T22:08:25ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762010-06-01281327133110.5194/angeo-28-1327-2010The Alfvén edge in asymmetric reconnectionA. Vaivads0A. Retinò1Yu. V. Khotyaintsev2M. André3Swedish Institute of Space Physics, Uppsala, P.O. Box 537, 751 21 Uppsala, SwedenSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSwedish Institute of Space Physics, Uppsala, P.O. Box 537, 751 21 Uppsala, SwedenSwedish Institute of Space Physics, Uppsala, P.O. Box 537, 751 21 Uppsala, SwedenWe show that in the case of magnetic reconnection where the Alfvén velocity is much higher in the plasma on one side of the current sheet than the other, an Alfvén edge is formed. This edge is located between the electron and ion edges on the high Alfvén velocity side of the current sheet. The Alfvén edge forms because the Alfvén wave generated near the X-line will propagate faster than the accelerated ions forming the ion edge. We discuss possible generation mechanism and the polarization of the Alfvén wave in the case when higher Alfvén speed is due to larger magnetic field and smaller plasma density, as in the case of magnetopause reconnection. The Alfvén wave can be generated due to Hall dynamics near the X-line. The Alfvén wave pulse has a unipolar electric field and the parallel current will be such that the outer current on the high magnetic field side is flowing away from the X-line. Understanding Alfvén edges is important for understanding the separatrix regions at the boundaries of reconnection jets. We present an example of Alfvén edge observed by the Cluster spacecraft at the magnetopause.https://www.ann-geophys.net/28/1327/2010/angeo-28-1327-2010.pdf
spellingShingle A. Vaivads
A. Retinò
Yu. V. Khotyaintsev
M. André
The Alfvén edge in asymmetric reconnection
Annales Geophysicae
title The Alfvén edge in asymmetric reconnection
title_full The Alfvén edge in asymmetric reconnection
title_fullStr The Alfvén edge in asymmetric reconnection
title_full_unstemmed The Alfvén edge in asymmetric reconnection
title_short The Alfvén edge in asymmetric reconnection
title_sort alfven edge in asymmetric reconnection
url https://www.ann-geophys.net/28/1327/2010/angeo-28-1327-2010.pdf
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