Simultaneous optical and radar signatures of poleward-moving auroral forms

Dayside poleward moving auroral forms (PMAFs) were detected between 06:30 and 07:00 UT on December 16, 1998, by the meridian scanning photometer and the all-sky camera at Ny Ålesund, Svalbard. Simultaneous SuperDARN HF radar measurements permitted the study of the associated ionospheric velocity pat...

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Published in:Annales Geophysicae
Main Authors: A. Thorolfsson, J.-C. Cerisier, M. Lockwood, P. E. Sandholt, C. Senior, M. Lester
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2000
Subjects:
Q
Online Access:https://doi.org/10.1007/s00585-000-1054-2
https://doaj.org/article/9b3a0b0ff6e54794b8eb7966b1aee0fd
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spelling ftdoajarticles:oai:doaj.org/article:9b3a0b0ff6e54794b8eb7966b1aee0fd 2023-05-15T17:48:28+02:00 Simultaneous optical and radar signatures of poleward-moving auroral forms A. Thorolfsson J.-C. Cerisier M. Lockwood P. E. Sandholt C. Senior M. Lester 2000-09-01T00:00:00Z https://doi.org/10.1007/s00585-000-1054-2 https://doaj.org/article/9b3a0b0ff6e54794b8eb7966b1aee0fd EN eng Copernicus Publications https://www.ann-geophys.net/18/1054/2000/angeo-18-1054-2000.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.1007/s00585-000-1054-2 0992-7689 1432-0576 https://doaj.org/article/9b3a0b0ff6e54794b8eb7966b1aee0fd Annales Geophysicae, Vol 18, Pp 1054-1066 (2000) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2000 ftdoajarticles https://doi.org/10.1007/s00585-000-1054-2 2022-12-31T03:27:27Z Dayside poleward moving auroral forms (PMAFs) were detected between 06:30 and 07:00 UT on December 16, 1998, by the meridian scanning photometer and the all-sky camera at Ny Ålesund, Svalbard. Simultaneous SuperDARN HF radar measurements permitted the study of the associated ionospheric velocity pattern. A good general agreement is observed between the location and movement of velocity enhancements (flow channels) and the PMAFs. Clear signatures of equatorward flow were detected in the vicinity of PMAFs. This flow is believed to be the signature of a return flow outside the reconnected flux tube, as predicted by the Southwood model. The simulated signatures of this model reproduce globally the measured signatures, and differences with the experimental data can be explained by the simplifications of the model. Proposed schemes of the flow modification due to the presence of several flow channels and the modification of cusp and region 1 field-aligned currents at the time of sporadic reconnection events are shown to fit well with the observations. Key words: Ionosphere (auroral ionosphere; plasma convection) - Magnetospheric physics (magnetopause; cusp and boundary layers) Article in Journal/Newspaper Ny Ålesund Ny-Ålesund Svalbard Directory of Open Access Journals: DOAJ Articles Ny-Ålesund Svalbard Annales Geophysicae 18 9 1054 1066
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
A. Thorolfsson
J.-C. Cerisier
M. Lockwood
P. E. Sandholt
C. Senior
M. Lester
Simultaneous optical and radar signatures of poleward-moving auroral forms
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description Dayside poleward moving auroral forms (PMAFs) were detected between 06:30 and 07:00 UT on December 16, 1998, by the meridian scanning photometer and the all-sky camera at Ny Ålesund, Svalbard. Simultaneous SuperDARN HF radar measurements permitted the study of the associated ionospheric velocity pattern. A good general agreement is observed between the location and movement of velocity enhancements (flow channels) and the PMAFs. Clear signatures of equatorward flow were detected in the vicinity of PMAFs. This flow is believed to be the signature of a return flow outside the reconnected flux tube, as predicted by the Southwood model. The simulated signatures of this model reproduce globally the measured signatures, and differences with the experimental data can be explained by the simplifications of the model. Proposed schemes of the flow modification due to the presence of several flow channels and the modification of cusp and region 1 field-aligned currents at the time of sporadic reconnection events are shown to fit well with the observations. Key words: Ionosphere (auroral ionosphere; plasma convection) - Magnetospheric physics (magnetopause; cusp and boundary layers)
format Article in Journal/Newspaper
author A. Thorolfsson
J.-C. Cerisier
M. Lockwood
P. E. Sandholt
C. Senior
M. Lester
author_facet A. Thorolfsson
J.-C. Cerisier
M. Lockwood
P. E. Sandholt
C. Senior
M. Lester
author_sort A. Thorolfsson
title Simultaneous optical and radar signatures of poleward-moving auroral forms
title_short Simultaneous optical and radar signatures of poleward-moving auroral forms
title_full Simultaneous optical and radar signatures of poleward-moving auroral forms
title_fullStr Simultaneous optical and radar signatures of poleward-moving auroral forms
title_full_unstemmed Simultaneous optical and radar signatures of poleward-moving auroral forms
title_sort simultaneous optical and radar signatures of poleward-moving auroral forms
publisher Copernicus Publications
publishDate 2000
url https://doi.org/10.1007/s00585-000-1054-2
https://doaj.org/article/9b3a0b0ff6e54794b8eb7966b1aee0fd
geographic Ny-Ålesund
Svalbard
geographic_facet Ny-Ålesund
Svalbard
genre Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
op_source Annales Geophysicae, Vol 18, Pp 1054-1066 (2000)
op_relation https://www.ann-geophys.net/18/1054/2000/angeo-18-1054-2000.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.1007/s00585-000-1054-2
0992-7689
1432-0576
https://doaj.org/article/9b3a0b0ff6e54794b8eb7966b1aee0fd
op_doi https://doi.org/10.1007/s00585-000-1054-2
container_title Annales Geophysicae
container_volume 18
container_issue 9
container_start_page 1054
op_container_end_page 1066
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