A statistical and event study of magnetotail dipolarization fronts

A study of dipolarization fronts of the Earth's magnetotail has been performed using seven years (2001–2007) of Cluster data. Events both with and without high-speed earthward flows are included. A superposed epoch analysis of the data shows that the dipolarization is preceeded by a decrease...

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Main Authors: D. Schmid, M. Volwerk, R. Nakamura, W. Baumjohann, M. Heyn
Format: Article
Language:English
Published: Copernicus Publications 2011-09-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/29/1537/2011/angeo-29-1537-2011.pdf
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spelling doaj-6484bb0359ef4e6dbbc1d4eb864f3acf2020-11-24T22:39:46ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762011-09-01291537154710.5194/angeo-29-1537-2011A statistical and event study of magnetotail dipolarization frontsD. Schmid0D. Schmid1M. Volwerk2R. Nakamura3W. Baumjohann4M. Heyn5Space Research Institute, Austrian Academy of Sciences, 8042 Graz, AustriaInstitute for Theoretical Physics, Technical University Graz, 8010 Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, 8042 Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, 8042 Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, 8042 Graz, AustriaInstitute for Theoretical Physics, Technical University Graz, 8010 Graz, AustriaA study of dipolarization fronts of the Earth's magnetotail has been performed using seven years (2001–2007) of Cluster data. Events both with and without high-speed earthward flows are included. A superposed epoch analysis of the data shows that the dipolarization is preceeded by a decrease of <I>B</I><sub>z</sub> before the increase. The duration of the dipolarization tends to be decreasing with increasing velocity of the plasma flows. The thickness of the dipolarization front is on average 1.8 plasma inertial lengths, independent of the plasma velocity. We find that the events fall into two categories: Earthward and tailward moving dipolarizations. The dipolarization fronts can be assumed to be tangential discontinuities and the currents on the front have mainly a perpendicular component.https://www.ann-geophys.net/29/1537/2011/angeo-29-1537-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Schmid
D. Schmid
M. Volwerk
R. Nakamura
W. Baumjohann
M. Heyn
spellingShingle D. Schmid
D. Schmid
M. Volwerk
R. Nakamura
W. Baumjohann
M. Heyn
A statistical and event study of magnetotail dipolarization fronts
Annales Geophysicae
author_facet D. Schmid
D. Schmid
M. Volwerk
R. Nakamura
W. Baumjohann
M. Heyn
author_sort D. Schmid
title A statistical and event study of magnetotail dipolarization fronts
title_short A statistical and event study of magnetotail dipolarization fronts
title_full A statistical and event study of magnetotail dipolarization fronts
title_fullStr A statistical and event study of magnetotail dipolarization fronts
title_full_unstemmed A statistical and event study of magnetotail dipolarization fronts
title_sort statistical and event study of magnetotail dipolarization fronts
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2011-09-01
description A study of dipolarization fronts of the Earth's magnetotail has been performed using seven years (2001–2007) of Cluster data. Events both with and without high-speed earthward flows are included. A superposed epoch analysis of the data shows that the dipolarization is preceeded by a decrease of <I>B</I><sub>z</sub> before the increase. The duration of the dipolarization tends to be decreasing with increasing velocity of the plasma flows. The thickness of the dipolarization front is on average 1.8 plasma inertial lengths, independent of the plasma velocity. We find that the events fall into two categories: Earthward and tailward moving dipolarizations. The dipolarization fronts can be assumed to be tangential discontinuities and the currents on the front have mainly a perpendicular component.
url https://www.ann-geophys.net/29/1537/2011/angeo-29-1537-2011.pdf
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