Statistical study of high-latitude plasma flow during magnetospheric substorms

We have utilised the near-global imaging capabilities of the Northern Hemisphere SuperDARN radars, to perform a statistical superposed epoch analysis of high-latitude plasma flows during magnetospheric substorms. The study involved 67 substorms, identified using the IMAGE FUV space-borne auroral...

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Main Authors: G. Provan, M. Lester, S. B. Mende, S. E. Milan
Format: Article
Language:English
Published: Copernicus Publications 2004-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/3607/2004/angeo-22-3607-2004.pdf
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author G. Provan
M. Lester
S. B. Mende
S. E. Milan
author_facet G. Provan
M. Lester
S. B. Mende
S. E. Milan
author_sort G. Provan
collection DOAJ
description We have utilised the near-global imaging capabilities of the Northern Hemisphere SuperDARN radars, to perform a statistical superposed epoch analysis of high-latitude plasma flows during magnetospheric substorms. The study involved 67 substorms, identified using the IMAGE FUV space-borne auroral imager. A substorm co-ordinate system was developed, centred on the magnetic local time and magnetic latitude of substorm onset determined from the auroral images. The plasma flow vectors from all 67 intervals were combined, creating global statistical plasma flow patterns and backscatter occurrence statistics during the substorm growth and expansion phases. The commencement of the substorm growth phase was clearly observed in the radar data 18-20min before substorm onset, with an increase in the anti-sunward component of the plasma velocity flowing across dawn sector of the polar cap and a peak in the dawn-to-dusk transpolar voltage. Nightside backscatter moved to lower latitudes as the growth phase progressed. At substorm onset a flow suppression region was observed on the nightside, with fast flows surrounding the suppressed flow region. The dawn-to-dusk transpolar voltage increased from ~40kV just before substorm onset to ~75kV 12min after onset. The low-latitude return flow started to increase at substorm onset and continued to increase until 8min after onset. The velocity flowing across the polar-cap peaked 12-14min after onset. This increase in the flux of the polar cap and the excitation of large-scale plasma flow occurred even though the IMF <i>B<sub>z</sub></i> component was increasing (becoming less negative) during most of this time. This study is the first to statistically prove that nightside reconnection creates magnetic flux and excites high-latitude plasma flow in a similar way to dayside reconnection and that dayside and nightside reconnection, are two separate time-dependent processes.
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spelling doaj.art-07f42f5542384e758e7f10abe5bb3b8f2022-12-22T03:13:02ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-11-01223607362410.5194/angeo-22-3607-2004Statistical study of high-latitude plasma flow during magnetospheric substormsG. Provan0M. Lester1S. B. Mende2S. E. Milan3Department of Physics and Astronomy, University of Leicester, University Road, Leicester, LE1 7RH, UKDepartment of Physics and Astronomy, University of Leicester, University Road, Leicester, LE1 7RH, UKSpace Science Laboratory, University of California, Berkeley, California, USADepartment of Physics and Astronomy, University of Leicester, University Road, Leicester, LE1 7RH, UKWe have utilised the near-global imaging capabilities of the Northern Hemisphere SuperDARN radars, to perform a statistical superposed epoch analysis of high-latitude plasma flows during magnetospheric substorms. The study involved 67 substorms, identified using the IMAGE FUV space-borne auroral imager. A substorm co-ordinate system was developed, centred on the magnetic local time and magnetic latitude of substorm onset determined from the auroral images. The plasma flow vectors from all 67 intervals were combined, creating global statistical plasma flow patterns and backscatter occurrence statistics during the substorm growth and expansion phases. The commencement of the substorm growth phase was clearly observed in the radar data 18-20min before substorm onset, with an increase in the anti-sunward component of the plasma velocity flowing across dawn sector of the polar cap and a peak in the dawn-to-dusk transpolar voltage. Nightside backscatter moved to lower latitudes as the growth phase progressed. At substorm onset a flow suppression region was observed on the nightside, with fast flows surrounding the suppressed flow region. The dawn-to-dusk transpolar voltage increased from ~40kV just before substorm onset to ~75kV 12min after onset. The low-latitude return flow started to increase at substorm onset and continued to increase until 8min after onset. The velocity flowing across the polar-cap peaked 12-14min after onset. This increase in the flux of the polar cap and the excitation of large-scale plasma flow occurred even though the IMF <i>B<sub>z</sub></i> component was increasing (becoming less negative) during most of this time. This study is the first to statistically prove that nightside reconnection creates magnetic flux and excites high-latitude plasma flow in a similar way to dayside reconnection and that dayside and nightside reconnection, are two separate time-dependent processes.https://www.ann-geophys.net/22/3607/2004/angeo-22-3607-2004.pdf
spellingShingle G. Provan
M. Lester
S. B. Mende
S. E. Milan
Statistical study of high-latitude plasma flow during magnetospheric substorms
Annales Geophysicae
title Statistical study of high-latitude plasma flow during magnetospheric substorms
title_full Statistical study of high-latitude plasma flow during magnetospheric substorms
title_fullStr Statistical study of high-latitude plasma flow during magnetospheric substorms
title_full_unstemmed Statistical study of high-latitude plasma flow during magnetospheric substorms
title_short Statistical study of high-latitude plasma flow during magnetospheric substorms
title_sort statistical study of high latitude plasma flow during magnetospheric substorms
url https://www.ann-geophys.net/22/3607/2004/angeo-22-3607-2004.pdf
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