Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions

We present multi-instrument observations using the meridian scanning photometer (MSP) at NyAlesund, the EISCAT Svalbard radar (ESR) and the CUTLASS Finland HF radar, to investigate the dynamics of the cusp region during pulsed reconnection events. The optical data obtained from the MSP indic...

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Main Authors: H. Khan, M. Lester, J. A. Davies, S. E. Milan, P. E. Sandholt
Format: Article
Language:English
Published: Copernicus Publications 2003-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/21/693/2003/angeo-21-693-2003.pdf
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spelling doaj-d2339240441847268a1c60a3dca16aa42020-11-24T23:34:42ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762003-03-012169370810.5194/angeo-21-693-2003Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditionsH. Khan0M. Lester1J. A. Davies2S. E. Milan3P. E. Sandholt4NASA Goddard Space Flight Center, Interplanetary Physics Branch, Greenbelt, MD 20771, USAUniversity of Leicester, Leicester, LE1 7RH, UKUniversity of Leicester, Leicester, LE1 7RH, UKUniversity of Leicester, Leicester, LE1 7RH, UKUniversity of Oslo, Oslo, NorwayWe present multi-instrument observations using the meridian scanning photometer (MSP) at NyAlesund, the EISCAT Svalbard radar (ESR) and the CUTLASS Finland HF radar, to investigate the dynamics of the cusp region during pulsed reconnection events. The optical data obtained from the MSP indicate the presence of several poleward-moving auroral forms (PMAFs) which have been previously identified as the auroral signature of pulsed reconnection. Furthermore, the optical green line (557.7 nm) luminosity indicates a loss of emission equatorward of the location of the onset of the PMAFs, characteristic of magnetospheric plasma escaping to the magnetosheath along newly opened field lines. This reduction in green line luminosity creates a &quot;dark region&quot;, the equatorward edge of which is found to lie close to the boundary between high and low spectral widths observed by the CUTLASS Finland radar. High spectral widths on the dayside have previously been identified as a good indicator of cusp backscatter. Both of these boundaries have been suggested to provide an accurate representation of the location of the open/closed field line boundary. The ESR observations show enhancements in electron density and electron temperature occurring in conjunction with the optical PMAFs. The observations demonstrate some correspondence with the theoretical predictions of Davis and Lockwood (1996), who used an auroral precipitation model to predict ESR observations in the vicinity of the cusp. However, the limitations of this model are apparent under conditions of large plasma flows in the ionosphere. Finally, convection velocities obtained from the HF radar data illustrate a flow regime similar to that predicted to be driven by strong IMF <i>B<sub>y</sub></i>, as described by Cowley and Lockwood (1992), demonstrating an initial azimuthal flow followed by a rotation to more poleward directions.<br><br><b>Key words. </b>Ionosphere (ionosphere-magnetosphere interactions; particle precipitation) – Magnetospheric physics (magnetopause, cusp and boundary layers)https://www.ann-geophys.net/21/693/2003/angeo-21-693-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Khan
M. Lester
J. A. Davies
S. E. Milan
P. E. Sandholt
spellingShingle H. Khan
M. Lester
J. A. Davies
S. E. Milan
P. E. Sandholt
Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
Annales Geophysicae
author_facet H. Khan
M. Lester
J. A. Davies
S. E. Milan
P. E. Sandholt
author_sort H. Khan
title Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
title_short Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
title_full Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
title_fullStr Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
title_full_unstemmed Multi-instrument study of the dynamic cusp during dominant IMF <i>B<sub>y</sub></i> conditions
title_sort multi-instrument study of the dynamic cusp during dominant imf <i>b<sub>y</sub></i> conditions
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2003-03-01
description We present multi-instrument observations using the meridian scanning photometer (MSP) at NyAlesund, the EISCAT Svalbard radar (ESR) and the CUTLASS Finland HF radar, to investigate the dynamics of the cusp region during pulsed reconnection events. The optical data obtained from the MSP indicate the presence of several poleward-moving auroral forms (PMAFs) which have been previously identified as the auroral signature of pulsed reconnection. Furthermore, the optical green line (557.7 nm) luminosity indicates a loss of emission equatorward of the location of the onset of the PMAFs, characteristic of magnetospheric plasma escaping to the magnetosheath along newly opened field lines. This reduction in green line luminosity creates a &quot;dark region&quot;, the equatorward edge of which is found to lie close to the boundary between high and low spectral widths observed by the CUTLASS Finland radar. High spectral widths on the dayside have previously been identified as a good indicator of cusp backscatter. Both of these boundaries have been suggested to provide an accurate representation of the location of the open/closed field line boundary. The ESR observations show enhancements in electron density and electron temperature occurring in conjunction with the optical PMAFs. The observations demonstrate some correspondence with the theoretical predictions of Davis and Lockwood (1996), who used an auroral precipitation model to predict ESR observations in the vicinity of the cusp. However, the limitations of this model are apparent under conditions of large plasma flows in the ionosphere. Finally, convection velocities obtained from the HF radar data illustrate a flow regime similar to that predicted to be driven by strong IMF <i>B<sub>y</sub></i>, as described by Cowley and Lockwood (1992), demonstrating an initial azimuthal flow followed by a rotation to more poleward directions.<br><br><b>Key words. </b>Ionosphere (ionosphere-magnetosphere interactions; particle precipitation) – Magnetospheric physics (magnetopause, cusp and boundary layers)
url https://www.ann-geophys.net/21/693/2003/angeo-21-693-2003.pdf
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