Dipolarization fronts in the near-Earth space and substorm dynamics

During magnetospheric substorms and plasma transport in the Earth's magnetotail various magnetic structures can be detected. Dipolarization fronts and flux ropes are the most prominent structures characteristic for substorm dynamics. However, they are treated as separate magnetotail features...

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Main Authors: I. I. Vogiatzis, A. Isavnin, Q.-G. Zong, E. T. Sarris, S. W. Lu, A. M. Tian
Format: Article
Language:English
Published: Copernicus Publications 2015-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/33/63/2015/angeo-33-63-2015.pdf
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spelling doaj-df1fe464b5e04a26b86468d6089f16952020-11-24T22:53:46ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762015-01-0133637410.5194/angeo-33-63-2015Dipolarization fronts in the near-Earth space and substorm dynamicsI. I. Vogiatzis0I. I. Vogiatzis1A. Isavnin2Q.-G. Zong3E. T. Sarris4S. W. Lu5A. M. Tian6Department of Electrical and Computer Engineering, Democritus University of Thrace, Xanthi, GreeceInstitute of Space Physics and Applied Technology, Peking University, Beijing, ChinaDepartment of Physics, University of Helsinki, P.O. Box 64, 00014, FinlandInstitute of Space Physics and Applied Technology, Peking University, Beijing, ChinaDepartment of Electrical and Computer Engineering, Democritus University of Thrace, Xanthi, GreeceInstitute of Space Physics and Applied Technology, Peking University, Beijing, ChinaSchool of Space Science and Physics, Shandong University, Weihai, ChinaDuring magnetospheric substorms and plasma transport in the Earth's magnetotail various magnetic structures can be detected. Dipolarization fronts and flux ropes are the most prominent structures characteristic for substorm dynamics. However, they are treated as separate magnetotail features independent of each other. In this paper, we analyze a number of dipolarization fronts observed by the THEMIS (Time History of Events and Macroscale Interactions during Substorms) spacecraft at different geocentric distances by applying the magnetohydrostatic Grad–Shafranov (GS) reconstruction technique. Our analysis shows that there is a possibility of dipolarization fronts to originate from highly dissipated flux ropes which are in the late stage of their evolution, subjected to a continuous magnetic deterioration due to the reconnection process. These results may improve our understanding of magnetoplasma processes in Earth's magnetotail.https://www.ann-geophys.net/33/63/2015/angeo-33-63-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. I. Vogiatzis
I. I. Vogiatzis
A. Isavnin
Q.-G. Zong
E. T. Sarris
S. W. Lu
A. M. Tian
spellingShingle I. I. Vogiatzis
I. I. Vogiatzis
A. Isavnin
Q.-G. Zong
E. T. Sarris
S. W. Lu
A. M. Tian
Dipolarization fronts in the near-Earth space and substorm dynamics
Annales Geophysicae
author_facet I. I. Vogiatzis
I. I. Vogiatzis
A. Isavnin
Q.-G. Zong
E. T. Sarris
S. W. Lu
A. M. Tian
author_sort I. I. Vogiatzis
title Dipolarization fronts in the near-Earth space and substorm dynamics
title_short Dipolarization fronts in the near-Earth space and substorm dynamics
title_full Dipolarization fronts in the near-Earth space and substorm dynamics
title_fullStr Dipolarization fronts in the near-Earth space and substorm dynamics
title_full_unstemmed Dipolarization fronts in the near-Earth space and substorm dynamics
title_sort dipolarization fronts in the near-earth space and substorm dynamics
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2015-01-01
description During magnetospheric substorms and plasma transport in the Earth's magnetotail various magnetic structures can be detected. Dipolarization fronts and flux ropes are the most prominent structures characteristic for substorm dynamics. However, they are treated as separate magnetotail features independent of each other. In this paper, we analyze a number of dipolarization fronts observed by the THEMIS (Time History of Events and Macroscale Interactions during Substorms) spacecraft at different geocentric distances by applying the magnetohydrostatic Grad–Shafranov (GS) reconstruction technique. Our analysis shows that there is a possibility of dipolarization fronts to originate from highly dissipated flux ropes which are in the late stage of their evolution, subjected to a continuous magnetic deterioration due to the reconnection process. These results may improve our understanding of magnetoplasma processes in Earth's magnetotail.
url https://www.ann-geophys.net/33/63/2015/angeo-33-63-2015.pdf
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