Wind observations of low energy particles within a solar wind reconnection region

We report characteristics of thermal particle observations during the encounter of the Wind satellite with the separatrix and the outflow domains of a reconnection event on 22 July 1999 in the solar wind. During the studied event the electrostatic analyzers on Wind were transmitting three-dimens...

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Main Authors: K. E. J. Huttunen, S. D. Bale, C. Salem
Format: Article
Language:English
Published: Copernicus Publications 2008-09-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/2701/2008/angeo-26-2701-2008.pdf
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spelling doaj-4d0e93df072e45538eec487e1d8eeacb2020-11-25T00:02:52ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-09-01262701271010.5194/angeo-26-2701-2008Wind observations of low energy particles within a solar wind reconnection regionK. E. J. Huttunen0K. E. J. Huttunen1S. D. Bale2S. D. Bale3C. Salem4Space Sciences Laboratory, University of California, 7 Gauss Way, Berkeley, CA 94720, USADepartment of Physics, P.O. Box 64, 00014, Univeristy of Helsinki, FinlandSpace Sciences Laboratory, University of California, 7 Gauss Way, Berkeley, CA 94720, USADepartment of Physics, University of California, Berkeley, CA 94720, USASpace Sciences Laboratory, University of California, 7 Gauss Way, Berkeley, CA 94720, USAWe report characteristics of thermal particle observations during the encounter of the Wind satellite with the separatrix and the outflow domains of a reconnection event on 22 July 1999 in the solar wind. During the studied event the electrostatic analyzers on Wind were transmitting three-dimensional electron and proton distributions in a burst mode every 3 s, the spin period of the spacecraft. The event was associated with a magnetic shear angle of 114° and a large guide magnetic field. The observations suggest that Wind crossed the separatrix and outflow regions about a thousand of ion skin depths from the X-line. At the leading separator boundary, a strong proton beam was identified that originated from the direction of the X-line. In the separatrix and the outflow regions, the phase space distributions of thermal electrons displayed field aligned bidirectional anisotropy. During the crossings of the current sheets bounding the outflow region, we identified two adjacent layers in which the dominant thermal electron flows were towards the X-line at the inner edges of the current sheets and away from the X-line at the outer edges. Interestingly, simulation studies and observations in the Earth's magnetosphere have revealed that the electron flows are reversed, consistent with the Hall current system.https://www.ann-geophys.net/26/2701/2008/angeo-26-2701-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. E. J. Huttunen
K. E. J. Huttunen
S. D. Bale
S. D. Bale
C. Salem
spellingShingle K. E. J. Huttunen
K. E. J. Huttunen
S. D. Bale
S. D. Bale
C. Salem
Wind observations of low energy particles within a solar wind reconnection region
Annales Geophysicae
author_facet K. E. J. Huttunen
K. E. J. Huttunen
S. D. Bale
S. D. Bale
C. Salem
author_sort K. E. J. Huttunen
title Wind observations of low energy particles within a solar wind reconnection region
title_short Wind observations of low energy particles within a solar wind reconnection region
title_full Wind observations of low energy particles within a solar wind reconnection region
title_fullStr Wind observations of low energy particles within a solar wind reconnection region
title_full_unstemmed Wind observations of low energy particles within a solar wind reconnection region
title_sort wind observations of low energy particles within a solar wind reconnection region
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-09-01
description We report characteristics of thermal particle observations during the encounter of the Wind satellite with the separatrix and the outflow domains of a reconnection event on 22 July 1999 in the solar wind. During the studied event the electrostatic analyzers on Wind were transmitting three-dimensional electron and proton distributions in a burst mode every 3 s, the spin period of the spacecraft. The event was associated with a magnetic shear angle of 114° and a large guide magnetic field. The observations suggest that Wind crossed the separatrix and outflow regions about a thousand of ion skin depths from the X-line. At the leading separator boundary, a strong proton beam was identified that originated from the direction of the X-line. In the separatrix and the outflow regions, the phase space distributions of thermal electrons displayed field aligned bidirectional anisotropy. During the crossings of the current sheets bounding the outflow region, we identified two adjacent layers in which the dominant thermal electron flows were towards the X-line at the inner edges of the current sheets and away from the X-line at the outer edges. Interestingly, simulation studies and observations in the Earth's magnetosphere have revealed that the electron flows are reversed, consistent with the Hall current system.
url https://www.ann-geophys.net/26/2701/2008/angeo-26-2701-2008.pdf
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