Observations of significant flux closure by dual lobe reconnection

We present an interval of dual lobe reconnection during which interplanetary magnetic field lines are captured by the magnetosphere by reconnecting at high latitudes in both the Northern and the Southern Hemispheres. This event was identified using measurements of the ionospheric convection flow...

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Main Authors: S. M. Imber, S. E. Milan, B. Hubert
Format: Article
Language:English
Published: Copernicus Publications 2007-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/25/1617/2007/angeo-25-1617-2007.pdf
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spelling doaj-1088c625c3e74398876d63bae73d4f0d2020-11-24T22:02:18ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762007-07-01251617162710.5194/angeo-25-1617-2007Observations of significant flux closure by dual lobe reconnectionS. M. Imber0S. E. Milan1B. Hubert2Department of Physics and Astronomy, University of Leicester, Leicester, UKDepartment of Physics and Astronomy, University of Leicester, Leicester, UKInstitut d'Atmospherique et de Geophysique, Université de Liège, Liège, BelgiumWe present an interval of dual lobe reconnection during which interplanetary magnetic field lines are captured by the magnetosphere by reconnecting at high latitudes in both the Northern and the Southern Hemispheres. This event was identified using measurements of the ionospheric convection flow and observations of the aurora using the SuperDARN radars and the IMAGE spacecraft. A cusp spot, characteristic of northward IMF, is clearly visible for a 30 min period enabling the ionospheric footprint of the Northern Hemisphere merging gap to be accurately determined. During the interval a strong burst of sunward flow across the dayside open/closed field line boundary (OCB) is observed, which we interpret as the reconfiguration of the magnetosphere following a burst of reconnection. Noon-midnight and dawn-dusk keograms of the aurora show that the polar cap shrinks during the interval indicating that a large amount of flux was closed by the reconnection. Using the SuperDARN potential maps it is possible to calculate that the amount of flux closed during the interval is 0.13 GWb which represents approximately 10% of the pre-existing polar cap. The number of ions captured by the burst of dual lobe reconnection was calculated to be ~2.2&times;10<sup>31</sup>, more than sufficient to populate a cold, dense plasma sheet. That a dense plasma sheet was not subsequently observed is discussed in terms of subsequent changes in the IMF.https://www.ann-geophys.net/25/1617/2007/angeo-25-1617-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. M. Imber
S. E. Milan
B. Hubert
spellingShingle S. M. Imber
S. E. Milan
B. Hubert
Observations of significant flux closure by dual lobe reconnection
Annales Geophysicae
author_facet S. M. Imber
S. E. Milan
B. Hubert
author_sort S. M. Imber
title Observations of significant flux closure by dual lobe reconnection
title_short Observations of significant flux closure by dual lobe reconnection
title_full Observations of significant flux closure by dual lobe reconnection
title_fullStr Observations of significant flux closure by dual lobe reconnection
title_full_unstemmed Observations of significant flux closure by dual lobe reconnection
title_sort observations of significant flux closure by dual lobe reconnection
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2007-07-01
description We present an interval of dual lobe reconnection during which interplanetary magnetic field lines are captured by the magnetosphere by reconnecting at high latitudes in both the Northern and the Southern Hemispheres. This event was identified using measurements of the ionospheric convection flow and observations of the aurora using the SuperDARN radars and the IMAGE spacecraft. A cusp spot, characteristic of northward IMF, is clearly visible for a 30 min period enabling the ionospheric footprint of the Northern Hemisphere merging gap to be accurately determined. During the interval a strong burst of sunward flow across the dayside open/closed field line boundary (OCB) is observed, which we interpret as the reconfiguration of the magnetosphere following a burst of reconnection. Noon-midnight and dawn-dusk keograms of the aurora show that the polar cap shrinks during the interval indicating that a large amount of flux was closed by the reconnection. Using the SuperDARN potential maps it is possible to calculate that the amount of flux closed during the interval is 0.13 GWb which represents approximately 10% of the pre-existing polar cap. The number of ions captured by the burst of dual lobe reconnection was calculated to be ~2.2&times;10<sup>31</sup>, more than sufficient to populate a cold, dense plasma sheet. That a dense plasma sheet was not subsequently observed is discussed in terms of subsequent changes in the IMF.
url https://www.ann-geophys.net/25/1617/2007/angeo-25-1617-2007.pdf
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