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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2007-07-01
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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 ~2.2×10<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 ~2.2×10<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 |
work_keys_str_mv |
AT smimber observationsofsignificantfluxclosurebyduallobereconnection AT semilan observationsofsignificantfluxclosurebyduallobereconnection AT bhubert observationsofsignificantfluxclosurebyduallobereconnection |
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