Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail

On 13August 2002, at ~23:00UT, about 10 min after a substorm intensification, Cluster observes a flux rope in the central magnetotail, followed by a localised fast flow event about oneminute later. Associated with the flux rope event, a traveling compression region (TCR) is seen by those Cluster spa...

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Published in:Annales Geophysicae
Main Authors: O. Amm, R. Nakamura, H. U. Frey, Y. Ogawa, M. Kubyshkina, A. Balogh, H. Rème
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2006
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-24-735-2006
https://doaj.org/article/1817e988f52b4255a79a77556468a8ec
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spelling ftdoajarticles:oai:doaj.org/article:1817e988f52b4255a79a77556468a8ec 2023-05-15T16:04:50+02:00 Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail O. Amm R. Nakamura H. U. Frey Y. Ogawa M. Kubyshkina A. Balogh H. Rème 2006-03-01T00:00:00Z https://doi.org/10.5194/angeo-24-735-2006 https://doaj.org/article/1817e988f52b4255a79a77556468a8ec EN eng Copernicus Publications https://www.ann-geophys.net/24/735/2006/angeo-24-735-2006.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-24-735-2006 0992-7689 1432-0576 https://doaj.org/article/1817e988f52b4255a79a77556468a8ec Annales Geophysicae, Vol 24, Pp 735-750 (2006) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2006 ftdoajarticles https://doi.org/10.5194/angeo-24-735-2006 2022-12-31T04:15:57Z On 13August 2002, at ~23:00UT, about 10 min after a substorm intensification, Cluster observes a flux rope in the central magnetotail, followed by a localised fast flow event about oneminute later. Associated with the flux rope event, a traveling compression region (TCR) is seen by those Cluster spacecraft which reside in the lobe. In the conjugate ionospheric region in Northern Scandinavia, the MIRACLE network observes the ionospheric equivalent currents, and the electron densities and electric fields are measured by the EISCAT radar along a meridional scanning profile. Further, the auroral evolution is observed with the Wideband Imaging Camera (WIC) on the IMAGE satellite. We compare in detail the substorm evolution as observed in the ionosphere and in the magnetosphere, and examine whether topological correspondences to the flux rope event exist in the ionospheric signatures. The large-scale mapping of both the location and the direction of the flux rope to the ionosphere shows an excellent correspondence to a lens-shaped region of an auroral emission minimum. This region is bracketed by an auroral region equatorward of it which was preexisting to the substorm intensification, and a substorm-related auroral region poleward of it. It is characterised by reduced ionospheric conductances with respect to its environment, and downward field-aligned current (FAC) observed both in the magnetosphere and in the ionosphere. As determined from the ionospheric data, this downward FAC area is moving eastward with a speed of ~2 km s -1 , in good agreement with the mapped plasma bulk velocity measured at the Cluster satellite closest to that area. Further southwestward to this leading downward FAC area, a trailing upward FAC area is observed that moves eastward with the same speed. The direction of the ionospheric electric field permits a current closure between these two FAC areas through the ionosphere. We speculate that these FAC areas may correspond to the ends of the flux rope in its symmetry direction. Article in Journal/Newspaper EISCAT Directory of Open Access Journals: DOAJ Articles Annales Geophysicae 24 2 735 750
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
O. Amm
R. Nakamura
H. U. Frey
Y. Ogawa
M. Kubyshkina
A. Balogh
H. Rème
Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description On 13August 2002, at ~23:00UT, about 10 min after a substorm intensification, Cluster observes a flux rope in the central magnetotail, followed by a localised fast flow event about oneminute later. Associated with the flux rope event, a traveling compression region (TCR) is seen by those Cluster spacecraft which reside in the lobe. In the conjugate ionospheric region in Northern Scandinavia, the MIRACLE network observes the ionospheric equivalent currents, and the electron densities and electric fields are measured by the EISCAT radar along a meridional scanning profile. Further, the auroral evolution is observed with the Wideband Imaging Camera (WIC) on the IMAGE satellite. We compare in detail the substorm evolution as observed in the ionosphere and in the magnetosphere, and examine whether topological correspondences to the flux rope event exist in the ionospheric signatures. The large-scale mapping of both the location and the direction of the flux rope to the ionosphere shows an excellent correspondence to a lens-shaped region of an auroral emission minimum. This region is bracketed by an auroral region equatorward of it which was preexisting to the substorm intensification, and a substorm-related auroral region poleward of it. It is characterised by reduced ionospheric conductances with respect to its environment, and downward field-aligned current (FAC) observed both in the magnetosphere and in the ionosphere. As determined from the ionospheric data, this downward FAC area is moving eastward with a speed of ~2 km s -1 , in good agreement with the mapped plasma bulk velocity measured at the Cluster satellite closest to that area. Further southwestward to this leading downward FAC area, a trailing upward FAC area is observed that moves eastward with the same speed. The direction of the ionospheric electric field permits a current closure between these two FAC areas through the ionosphere. We speculate that these FAC areas may correspond to the ends of the flux rope in its symmetry direction.
format Article in Journal/Newspaper
author O. Amm
R. Nakamura
H. U. Frey
Y. Ogawa
M. Kubyshkina
A. Balogh
H. Rème
author_facet O. Amm
R. Nakamura
H. U. Frey
Y. Ogawa
M. Kubyshkina
A. Balogh
H. Rème
author_sort O. Amm
title Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
title_short Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
title_full Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
title_fullStr Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
title_full_unstemmed Substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
title_sort substorm topology in the ionosphere and magnetosphere during a flux rope event in the magnetotail
publisher Copernicus Publications
publishDate 2006
url https://doi.org/10.5194/angeo-24-735-2006
https://doaj.org/article/1817e988f52b4255a79a77556468a8ec
genre EISCAT
genre_facet EISCAT
op_source Annales Geophysicae, Vol 24, Pp 735-750 (2006)
op_relation https://www.ann-geophys.net/24/735/2006/angeo-24-735-2006.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-24-735-2006
0992-7689
1432-0576
https://doaj.org/article/1817e988f52b4255a79a77556468a8ec
op_doi https://doi.org/10.5194/angeo-24-735-2006
container_title Annales Geophysicae
container_volume 24
container_issue 2
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