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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2015-01-01
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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 |
work_keys_str_mv |
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