Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event

Line-of-sight Doppler velocities from the SuperDARN CUTLASS HF radar pair have been combined to produce the first two-dimensional vector measurements of the convection pattern throughout the ionospheric footprint of a flux transfer event (a pulsed ionospheric flow, or PIF). Very stable and moder...

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Main Authors: K. A. McWilliams, T. K. Yeoman, S. W. H. Cowley
Format: Article
Language:English
Published: Copernicus Publications 2000-12-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/18/1584/2000/angeo-18-1584-2000.pdf
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spelling doaj-9d6b1de68d1a42c5a62724dc5f06418d2020-11-24T22:26:40ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762000-12-01181584159810.1007/s00585-001-1584-2Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer eventK. A. McWilliams0T. K. Yeoman1S. W. H. Cowley2Department of Physics and Astronomy, Leicester University, University Road, Leicester LE1 7RH, UKDepartment of Physics and Astronomy, Leicester University, University Road, Leicester LE1 7RH, UKDepartment of Physics and Astronomy, Leicester University, University Road, Leicester LE1 7RH, UKLine-of-sight Doppler velocities from the SuperDARN CUTLASS HF radar pair have been combined to produce the first two-dimensional vector measurements of the convection pattern throughout the ionospheric footprint of a flux transfer event (a pulsed ionospheric flow, or PIF). Very stable and moderate interplanetary magnetic field conditions, along with a preceding prolonged period of northward interplanetary magnetic field, allow a detailed study of the spatial and the temporal evolution of the ionospheric response to magnetic reconnection. The flux tube footprint is tracked for half an hour across six hours of local time in the auroral zone, from magnetic local noon to dusk. The motion of the footprint of the newly reconnected flux tube is compared with the ionospheric convection velocity. Two primary intervals in the PIF's evolution have been determined. For the first half of its lifetime in the radar field of view the phase speed of the PIF is highly variable and the mean speed is nearly twice the ionospheric convection speed. For the final half of its lifetime the phase velocity becomes much less variable and slows down to the ionospheric convection velocity. The evolution of the flux tube in the magnetosphere has been studied using magnetic field, magnetopause and magnetosheath models. The data are consistent with an interval of azimuthally propagating magnetopause reconnection, in a manner consonant with a peeling of magnetic flux from the magnetopause, followed by an interval of anti-sunward convection of reconnected flux tubes.<br><br><b>Key words:</b> Magnetospheric physics (magnetosphere · ionosphere interactions; plasma convection; solar wind · magnetosphere interactions)https://www.ann-geophys.net/18/1584/2000/angeo-18-1584-2000.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. A. McWilliams
T. K. Yeoman
S. W. H. Cowley
spellingShingle K. A. McWilliams
T. K. Yeoman
S. W. H. Cowley
Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
Annales Geophysicae
author_facet K. A. McWilliams
T. K. Yeoman
S. W. H. Cowley
author_sort K. A. McWilliams
title Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
title_short Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
title_full Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
title_fullStr Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
title_full_unstemmed Two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
title_sort two-dimensional electric field measurements in the ionospheric footprint of a flux transfer event
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2000-12-01
description Line-of-sight Doppler velocities from the SuperDARN CUTLASS HF radar pair have been combined to produce the first two-dimensional vector measurements of the convection pattern throughout the ionospheric footprint of a flux transfer event (a pulsed ionospheric flow, or PIF). Very stable and moderate interplanetary magnetic field conditions, along with a preceding prolonged period of northward interplanetary magnetic field, allow a detailed study of the spatial and the temporal evolution of the ionospheric response to magnetic reconnection. The flux tube footprint is tracked for half an hour across six hours of local time in the auroral zone, from magnetic local noon to dusk. The motion of the footprint of the newly reconnected flux tube is compared with the ionospheric convection velocity. Two primary intervals in the PIF's evolution have been determined. For the first half of its lifetime in the radar field of view the phase speed of the PIF is highly variable and the mean speed is nearly twice the ionospheric convection speed. For the final half of its lifetime the phase velocity becomes much less variable and slows down to the ionospheric convection velocity. The evolution of the flux tube in the magnetosphere has been studied using magnetic field, magnetopause and magnetosheath models. The data are consistent with an interval of azimuthally propagating magnetopause reconnection, in a manner consonant with a peeling of magnetic flux from the magnetopause, followed by an interval of anti-sunward convection of reconnected flux tubes.<br><br><b>Key words:</b> Magnetospheric physics (magnetosphere · ionosphere interactions; plasma convection; solar wind · magnetosphere interactions)
url https://www.ann-geophys.net/18/1584/2000/angeo-18-1584-2000.pdf
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