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: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-997-1388-0
https://angeo.copernicus.org/articles/15/1388/1997/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo34269 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. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-997-1388-0 https://angeo.copernicus.org/articles/15/1388/1997/ eng eng doi:10.1007/s00585-997-1388-0 https://angeo.copernicus.org/articles/15/1388/1997/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-997-1388-0 2020-07-20T16:28:07Z 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. Text Ny Ålesund Ny-Ålesund Svalbard Copernicus Publications: E-Journals Ny-Ålesund Svalbard Annales Geophysicae 15 11 1388 1398
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
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.
format Text
author Milan, S. E.
Lester, M.
Moen, J.
spellingShingle Milan, S. E.
Lester, M.
Moen, J.
A comparison of optical and coherent HF radar backscatter observations of a post-midnight aurora
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
publishDate 2018
url https://doi.org/10.1007/s00585-997-1388-0
https://angeo.copernicus.org/articles/15/1388/1997/
geographic Ny-Ålesund
Svalbard
geographic_facet Ny-Ålesund
Svalbard
genre Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-997-1388-0
https://angeo.copernicus.org/articles/15/1388/1997/
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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