SABRE observations of structured ionospheric flows during substorm expansion phase onset

The irregularity velocity patterns observed by the SABRE coherent radar at substorm expansion phase onset, which is identified by magnetometer observations of Pi2 pulsations, are occasionally highly structured. In all the examples of structured velocity patterns examined, the SABRE viewing area is l...

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Main Authors: M. Lester, E. G. Bradshaw, T. B. Jones
Format: Article
Language:English
Published: Copernicus Publications
Series:Annales Geophysicae
Online Access:http://www.ann-geophys.net/12/1027/1994/angeo-12-1027-1994.html
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spelling doaj-bffeec722f8b428292f24118f156dc362020-11-24T21:21:53ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761210/1110271038SABRE observations of structured ionospheric flows during substorm expansion phase onsetM. LesterE. G. BradshawT. B. JonesThe irregularity velocity patterns observed by the SABRE coherent radar at substorm expansion phase onset, which is identified by magnetometer observations of Pi2 pulsations, are occasionally highly structured. In all the examples of structured velocity patterns examined, the SABRE viewing area is located at longitudes within the inferred substorm current wedge. Three types of structured velocity regime are apparent depending on the level of magnetic activity and the position of the radar viewing area relative to the substorm enhanced currents and the Pi2 pulsation generation region. Firstly, vortex-like velocity patterns are observed and these may be caused by the field-aligned currents associated with the substorm current wedge. Secondly, regions of equatorward velocity are also observed at times of substorm expansion phase onset moving longitudinally across the SABRE viewing area. The longitudinal movement is usually westward although an example of eastward motion has been observed. The phase velocity of these regions of equatorward flow is typically 1-3 km s<sup>-1</sup>. The observed equatorward velocities occur at the poleward edge or poleward of the background convection velocities observed by SABRE. These equatorward velocities may be related to the westward travelling surge and to the expansion (eastwards as well as westwards) of the brightening arc region at substorm onset. Thirdly, the flow rotates equatorward within the field of view but does not then appear to move longitudinally. These equatorward velocities may relate to the earthward surge of plasma from the magnetotail at substorm onset. http://www.ann-geophys.net/12/1027/1994/angeo-12-1027-1994.html
collection DOAJ
language English
format Article
sources DOAJ
author M. Lester
E. G. Bradshaw
T. B. Jones
spellingShingle M. Lester
E. G. Bradshaw
T. B. Jones
SABRE observations of structured ionospheric flows during substorm expansion phase onset
Annales Geophysicae
author_facet M. Lester
E. G. Bradshaw
T. B. Jones
author_sort M. Lester
title SABRE observations of structured ionospheric flows during substorm expansion phase onset
title_short SABRE observations of structured ionospheric flows during substorm expansion phase onset
title_full SABRE observations of structured ionospheric flows during substorm expansion phase onset
title_fullStr SABRE observations of structured ionospheric flows during substorm expansion phase onset
title_full_unstemmed SABRE observations of structured ionospheric flows during substorm expansion phase onset
title_sort sabre observations of structured ionospheric flows during substorm expansion phase onset
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
description The irregularity velocity patterns observed by the SABRE coherent radar at substorm expansion phase onset, which is identified by magnetometer observations of Pi2 pulsations, are occasionally highly structured. In all the examples of structured velocity patterns examined, the SABRE viewing area is located at longitudes within the inferred substorm current wedge. Three types of structured velocity regime are apparent depending on the level of magnetic activity and the position of the radar viewing area relative to the substorm enhanced currents and the Pi2 pulsation generation region. Firstly, vortex-like velocity patterns are observed and these may be caused by the field-aligned currents associated with the substorm current wedge. Secondly, regions of equatorward velocity are also observed at times of substorm expansion phase onset moving longitudinally across the SABRE viewing area. The longitudinal movement is usually westward although an example of eastward motion has been observed. The phase velocity of these regions of equatorward flow is typically 1-3 km s<sup>-1</sup>. The observed equatorward velocities occur at the poleward edge or poleward of the background convection velocities observed by SABRE. These equatorward velocities may be related to the westward travelling surge and to the expansion (eastwards as well as westwards) of the brightening arc region at substorm onset. Thirdly, the flow rotates equatorward within the field of view but does not then appear to move longitudinally. These equatorward velocities may relate to the earthward surge of plasma from the magnetotail at substorm onset.
url http://www.ann-geophys.net/12/1027/1994/angeo-12-1027-1994.html
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