Statistical study of auroral omega bands

The presence of very few statistical studies on auroral omega bands motivated us to test-use a semi-automatic method for identifying large-scale undulations of the diffuse aurora boundary and to investigate their occurrence. Five identical all-sky cameras with overlapping fields of view provided dat...

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Published in:Annales Geophysicae
Main Authors: Partamies, Noora, Weygand, James M., Juusola, Liisa
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-35-1069-2017
https://angeo.copernicus.org/articles/35/1069/2017/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo57835 2023-05-15T16:13:01+02:00 Statistical study of auroral omega bands Partamies, Noora Weygand, James M. Juusola, Liisa 2018-09-27 application/pdf https://doi.org/10.5194/angeo-35-1069-2017 https://angeo.copernicus.org/articles/35/1069/2017/ eng eng doi:10.5194/angeo-35-1069-2017 https://angeo.copernicus.org/articles/35/1069/2017/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-35-1069-2017 2020-07-20T16:23:37Z The presence of very few statistical studies on auroral omega bands motivated us to test-use a semi-automatic method for identifying large-scale undulations of the diffuse aurora boundary and to investigate their occurrence. Five identical all-sky cameras with overlapping fields of view provided data for 438 auroral omega-like structures over Fennoscandian Lapland from 1996 to 2007. The results from this set of omega band events agree remarkably well with previous observations of omega band occurrence in magnetic local time (MLT), lifetime, location between the region 1 and 2 field-aligned currents, as well as current density estimates. The average peak emission height of omega forms corresponds to the estimated precipitation energies of a few keV, which experienced no significant change during the events. Analysis of both local and global magnetic indices demonstrates that omega bands are observed during substorm expansion and recovery phases that are more intense than average substorm expansion and recovery phases in the same region. The omega occurrence with respect to the substorm expansion and recovery phases is in a very good agreement with an earlier observed distribution of fast earthward flows in the plasma sheet during expansion and recovery phases. These findings support the theory that omegas are produced by fast earthward flows and auroral streamers, despite the rarity of good conjugate observations. Text Fennoscandian Lapland Copernicus Publications: E-Journals Annales Geophysicae 35 5 1069 1083
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The presence of very few statistical studies on auroral omega bands motivated us to test-use a semi-automatic method for identifying large-scale undulations of the diffuse aurora boundary and to investigate their occurrence. Five identical all-sky cameras with overlapping fields of view provided data for 438 auroral omega-like structures over Fennoscandian Lapland from 1996 to 2007. The results from this set of omega band events agree remarkably well with previous observations of omega band occurrence in magnetic local time (MLT), lifetime, location between the region 1 and 2 field-aligned currents, as well as current density estimates. The average peak emission height of omega forms corresponds to the estimated precipitation energies of a few keV, which experienced no significant change during the events. Analysis of both local and global magnetic indices demonstrates that omega bands are observed during substorm expansion and recovery phases that are more intense than average substorm expansion and recovery phases in the same region. The omega occurrence with respect to the substorm expansion and recovery phases is in a very good agreement with an earlier observed distribution of fast earthward flows in the plasma sheet during expansion and recovery phases. These findings support the theory that omegas are produced by fast earthward flows and auroral streamers, despite the rarity of good conjugate observations.
format Text
author Partamies, Noora
Weygand, James M.
Juusola, Liisa
spellingShingle Partamies, Noora
Weygand, James M.
Juusola, Liisa
Statistical study of auroral omega bands
author_facet Partamies, Noora
Weygand, James M.
Juusola, Liisa
author_sort Partamies, Noora
title Statistical study of auroral omega bands
title_short Statistical study of auroral omega bands
title_full Statistical study of auroral omega bands
title_fullStr Statistical study of auroral omega bands
title_full_unstemmed Statistical study of auroral omega bands
title_sort statistical study of auroral omega bands
publishDate 2018
url https://doi.org/10.5194/angeo-35-1069-2017
https://angeo.copernicus.org/articles/35/1069/2017/
genre Fennoscandian
Lapland
genre_facet Fennoscandian
Lapland
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-35-1069-2017
https://angeo.copernicus.org/articles/35/1069/2017/
op_doi https://doi.org/10.5194/angeo-35-1069-2017
container_title Annales Geophysicae
container_volume 35
container_issue 5
container_start_page 1069
op_container_end_page 1083
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