A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora

A poleward-progressing 630 nm optical feature is observed between approximately 0100 UT and 0230 UT (0400 MLT to 0530 MLT) by a meridian-scanning photometer (MSP) located at Ny Ålesund, Svalbard. Simultaneous coherent HF radar measurements indicate a region of poleward-expanding backscatter with rap...

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Published in:Annales Geophysicae
Main Authors: Milan, S. E., Lester, M., Moen, J.
Format: Article in Journal/Newspaper
Language:English
Published: SPRINGER VERLAG 2012
Subjects:
Online Access:http://hdl.handle.net/2381/19757
http://www.ann-geophys.net/15/1388/1997/angeo-15-1388-1997.html
https://doi.org/10.1007/s00585-997-1388-0
id ftleicester:oai:lra.le.ac.uk:2381/19757
record_format openpolar
spelling ftleicester:oai:lra.le.ac.uk:2381/19757 2023-05-15T17:48:28+02:00 A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora Milan, S. E. Lester, M. Moen, J. 2012-10-24T09:07:34Z http://hdl.handle.net/2381/19757 http://www.ann-geophys.net/15/1388/1997/angeo-15-1388-1997.html https://doi.org/10.1007/s00585-997-1388-0 English eng SPRINGER VERLAG ANNALES GEOPHYSICAE-ATMOSPHERES HYDROSPHERES AND SPACE SCIENCES, 1997, 15 (11), pp. 1388-1398 0992-7689 http://hdl.handle.net/2381/19757 http://www.ann-geophys.net/15/1388/1997/angeo-15-1388-1997.html doi:10.1007/s00585-997-1388-0 Copyright © European Geosciences Union 1997 Web of Science http://webofknowledge.com Science & Technology Physical Sciences Astronomy & Astrophysics Geosciences Multidisciplinary Meteorology & Atmospheric Sciences Geology INTERPLANETARY MAGNETIC-FIELD SMALL-SCALE IRREGULARITIES LATITUDE F-REGION SUN-ALIGNED ARCS POLAR-CAP ELECTRIC-FIELD NORTHWARD CONVECTION PATTERNS TIMES Journal Article 2012 ftleicester https://doi.org/10.1007/s00585-997-1388-0 2019-03-22T20:17:01Z A poleward-progressing 630 nm optical feature is observed between approximately 0100 UT and 0230 UT (0400 MLT to 0530 MLT) by a meridian-scanning photometer (MSP) located at Ny Ålesund, Svalbard. Simultaneous coherent HF radar measurements indicate a region of poleward-expanding backscatter with rapid sunward plasma flow velocity along the MSP meridian. Spatial maps of the backscatter indicate a stationary backscatter feature aligned obliquely with respect to the MSP meridian, which produces an impression of poleward-expansion as the MSP progresses to later MLT. Two interpretations of the observations are possible, depending on whether the arc system is considered to move (time-dependent) or to be stationary in time and apparent motion is produced as the MSP meridian rotates underneath it (time-independent). The first interpretation is as a poleward motion of an east-west aligned auroral arc. In this case the appearance of the region of backscatter is not associated with the optical feature, though the velocities within it are enhanced when the two are co-located. The second interpretation is as a polar arc or theta aurora, common features of the polar cap under the prevailing IMF northwards conditions. In this case the backscatter appears as an approximately 150 km wide region adjacent to the optical arc. In both interpretations the luminosity of the optical feature appears related to the magnitude of the plasma flow velocity. The optical features presented here do not generate appreciable HF coherent backscatter, and are only identifiable in the backscatter data as a modification of the flow by the arc electrodynamics. 45599 Article in Journal/Newspaper Ny Ålesund Ny-Ålesund Svalbard University of Leicester: Leicester Research Archive (LRA) Svalbard Ny-Ålesund Annales Geophysicae 15 11 1388 1398
institution Open Polar
collection University of Leicester: Leicester Research Archive (LRA)
op_collection_id ftleicester
language English
topic Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
INTERPLANETARY MAGNETIC-FIELD
SMALL-SCALE IRREGULARITIES
LATITUDE F-REGION
SUN-ALIGNED ARCS
POLAR-CAP
ELECTRIC-FIELD
NORTHWARD
CONVECTION
PATTERNS
TIMES
spellingShingle Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
INTERPLANETARY MAGNETIC-FIELD
SMALL-SCALE IRREGULARITIES
LATITUDE F-REGION
SUN-ALIGNED ARCS
POLAR-CAP
ELECTRIC-FIELD
NORTHWARD
CONVECTION
PATTERNS
TIMES
Milan, S. E.
Lester, M.
Moen, J.
A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
topic_facet Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
INTERPLANETARY MAGNETIC-FIELD
SMALL-SCALE IRREGULARITIES
LATITUDE F-REGION
SUN-ALIGNED ARCS
POLAR-CAP
ELECTRIC-FIELD
NORTHWARD
CONVECTION
PATTERNS
TIMES
description A poleward-progressing 630 nm optical feature is observed between approximately 0100 UT and 0230 UT (0400 MLT to 0530 MLT) by a meridian-scanning photometer (MSP) located at Ny Ålesund, Svalbard. Simultaneous coherent HF radar measurements indicate a region of poleward-expanding backscatter with rapid sunward plasma flow velocity along the MSP meridian. Spatial maps of the backscatter indicate a stationary backscatter feature aligned obliquely with respect to the MSP meridian, which produces an impression of poleward-expansion as the MSP progresses to later MLT. Two interpretations of the observations are possible, depending on whether the arc system is considered to move (time-dependent) or to be stationary in time and apparent motion is produced as the MSP meridian rotates underneath it (time-independent). The first interpretation is as a poleward motion of an east-west aligned auroral arc. In this case the appearance of the region of backscatter is not associated with the optical feature, though the velocities within it are enhanced when the two are co-located. The second interpretation is as a polar arc or theta aurora, common features of the polar cap under the prevailing IMF northwards conditions. In this case the backscatter appears as an approximately 150 km wide region adjacent to the optical arc. In both interpretations the luminosity of the optical feature appears related to the magnitude of the plasma flow velocity. The optical features presented here do not generate appreciable HF coherent backscatter, and are only identifiable in the backscatter data as a modification of the flow by the arc electrodynamics. 45599
format Article in Journal/Newspaper
author Milan, S. E.
Lester, M.
Moen, J.
author_facet Milan, S. E.
Lester, M.
Moen, J.
author_sort Milan, S. E.
title A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
title_short A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
title_full A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
title_fullStr A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
title_full_unstemmed A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
title_sort comparison of optical and coherent hf radar backscatter observations of a post-midnight aurora
publisher SPRINGER VERLAG
publishDate 2012
url http://hdl.handle.net/2381/19757
http://www.ann-geophys.net/15/1388/1997/angeo-15-1388-1997.html
https://doi.org/10.1007/s00585-997-1388-0
geographic Svalbard
Ny-Ålesund
geographic_facet Svalbard
Ny-Ålesund
genre Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
op_source Web of Science
http://webofknowledge.com
op_relation ANNALES GEOPHYSICAE-ATMOSPHERES HYDROSPHERES AND SPACE SCIENCES, 1997, 15 (11), pp. 1388-1398
0992-7689
http://hdl.handle.net/2381/19757
http://www.ann-geophys.net/15/1388/1997/angeo-15-1388-1997.html
doi:10.1007/s00585-997-1388-0
op_rights Copyright © European Geosciences Union 1997
op_doi https://doi.org/10.1007/s00585-997-1388-0
container_title Annales Geophysicae
container_volume 15
container_issue 11
container_start_page 1388
op_container_end_page 1398
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