Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study

The dynamics of the cusp region and post-noon sector for an interval of predominantly IMF <i>B</i><sub>y</sub>, <i>B</i><sub>z</sub> &lt; 0 nT are studied with the CUTLASS Finland coherent HF radar, a meridian-scanning photometer located at Ny Å...

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Main Authors: S. E. Milan, M. Lester, S. W. H. Cowley, J. Moen, P. E. Sandholt, C. J. Owen
Format: Article
Language:English
Published: Copernicus Publications 1999-02-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/17/159/1999/angeo-17-159-1999.pdf
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spelling doaj-e9cdf83f2b954d8fa4dfb64b3be5635f2020-11-24T23:04:30ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761999-02-011715917210.1007/s00585-999-0159-5Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case studyS. E. Milan0M. Lester1S. W. H. Cowley2J. Moen3P. E. Sandholt4C. J. Owen5Department of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UKDepartment of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UKDepartment of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UKUNIS, P.O. Box 156, N-9170 Longyearbyen, NorwayDepartment of Physics, University of Oslo, P O Box 1048 Blindern, N-0316 Oslo, NorwayQueen Mary and Westfield College, University of London, London E1 4NS, UKThe dynamics of the cusp region and post-noon sector for an interval of predominantly IMF <i>B</i><sub>y</sub>, <i>B</i><sub>z</sub> &lt; 0 nT are studied with the CUTLASS Finland coherent HF radar, a meridian-scanning photometer located at Ny Ålesund, Svalbard, and a meridional network of magnetometers. The scanning mode of the radar is such that one beam is sampled every 14 s, and a 30° azimuthal sweep is completed every 2 minutes, all at 15 km range resolution. Both the radar backscatter and red line (630 nm) optical observations are closely co-located, especially at their equatorward boundary. The optical and radar aurora reveal three different behaviours which can interchange on the scale of minutes, and which are believed to be related to the dynamic nature of energy and momentum transfer from the solar wind to the magnetosphere through transient dayside reconnection. Two interpretations of the observations are presented, based upon the assumed location of the open/closed field line boundary (OCFLB). In the first, the OCFLB is co-located with equatorward boundary of the optical and radar aurora, placing most of the observations on open field lines. In the second, the observed aurora are interpreted as the ionospheric footprint of the region 1 current system, and the OCFLB is placed near the poleward edge of the radar backscatter and visible aurora; in this interpretation, most of the observations are placed on closed field lines, though transient brightenings of the optical aurora occur on open field lines. The observations reveal several transient features, including poleward and equatorward steps in the observed boundaries, &quot;braiding&quot; of the backscatter power, and 2 minute quasi-periodic enhancements of the plasma drift and optical intensity, predominantly on closed field lines.<br><br><b>Key words.</b> Ionosphere (auroral ionosphere; plasma convection) · Magnetospheric physics (magnetopause · cusp · and boundary layers)https://www.ann-geophys.net/17/159/1999/angeo-17-159-1999.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. E. Milan
M. Lester
S. W. H. Cowley
J. Moen
P. E. Sandholt
C. J. Owen
spellingShingle S. E. Milan
M. Lester
S. W. H. Cowley
J. Moen
P. E. Sandholt
C. J. Owen
Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
Annales Geophysicae
author_facet S. E. Milan
M. Lester
S. W. H. Cowley
J. Moen
P. E. Sandholt
C. J. Owen
author_sort S. E. Milan
title Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
title_short Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
title_full Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
title_fullStr Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
title_full_unstemmed Meridian-scanning photometer, coherent HF radar, and magnetometer observations of the cusp: a case study
title_sort meridian-scanning photometer, coherent hf radar, and magnetometer observations of the cusp: a case study
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1999-02-01
description The dynamics of the cusp region and post-noon sector for an interval of predominantly IMF <i>B</i><sub>y</sub>, <i>B</i><sub>z</sub> &lt; 0 nT are studied with the CUTLASS Finland coherent HF radar, a meridian-scanning photometer located at Ny Ålesund, Svalbard, and a meridional network of magnetometers. The scanning mode of the radar is such that one beam is sampled every 14 s, and a 30° azimuthal sweep is completed every 2 minutes, all at 15 km range resolution. Both the radar backscatter and red line (630 nm) optical observations are closely co-located, especially at their equatorward boundary. The optical and radar aurora reveal three different behaviours which can interchange on the scale of minutes, and which are believed to be related to the dynamic nature of energy and momentum transfer from the solar wind to the magnetosphere through transient dayside reconnection. Two interpretations of the observations are presented, based upon the assumed location of the open/closed field line boundary (OCFLB). In the first, the OCFLB is co-located with equatorward boundary of the optical and radar aurora, placing most of the observations on open field lines. In the second, the observed aurora are interpreted as the ionospheric footprint of the region 1 current system, and the OCFLB is placed near the poleward edge of the radar backscatter and visible aurora; in this interpretation, most of the observations are placed on closed field lines, though transient brightenings of the optical aurora occur on open field lines. The observations reveal several transient features, including poleward and equatorward steps in the observed boundaries, &quot;braiding&quot; of the backscatter power, and 2 minute quasi-periodic enhancements of the plasma drift and optical intensity, predominantly on closed field lines.<br><br><b>Key words.</b> Ionosphere (auroral ionosphere; plasma convection) · Magnetospheric physics (magnetopause · cusp · and boundary layers)
url https://www.ann-geophys.net/17/159/1999/angeo-17-159-1999.pdf
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