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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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 "dark region", 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 "dark region", 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 |
work_keys_str_mv |
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