Features of stable diffuse arcs observed by means of auroral tomography

In this paper we study the spatial distribution of optical volume emission rates and peculiarities of the luminosity intensity within weak diffuse auroral arcs recovered by means of auroral tomography. The tomographic images are obtained from sets of scanning multi-channel photometer data obtained i...

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Published in:Annales Geophysicae
Main Authors: Dashkevich, Zh. V., Ivanov, V. E., Khudukon, B. Z.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-25-1131-2007
https://angeo.copernicus.org/articles/25/1131/2007/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo36171 2023-05-15T17:05:00+02:00 Features of stable diffuse arcs observed by means of auroral tomography Dashkevich, Zh. V. Ivanov, V. E. Khudukon, B. Z. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-25-1131-2007 https://angeo.copernicus.org/articles/25/1131/2007/ eng eng doi:10.5194/angeo-25-1131-2007 https://angeo.copernicus.org/articles/25/1131/2007/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-25-1131-2007 2020-07-20T16:27:05Z In this paper we study the spatial distribution of optical volume emission rates and peculiarities of the luminosity intensity within weak diffuse auroral arcs recovered by means of auroral tomography. The tomographic images are obtained from sets of scanning multi-channel photometer data obtained in February 1999 on the Kola Peninsula in Russia at three sites of a chain extending 226 km along the geomagnetic meridian. The 427.8- and 557.7-nm emissions of a 15-s time resolution observed within one hour during low geomagnetic activity are analyzed. We found that the intensity profile of an individual arc along the geomagnetic meridian has an inverted-V-shape. The luminosity maximum altitude decrease by 4–14 km at about 140 km distance in the south-north direction can be observed during two or more diffuse arcs. The parameters of the precipitating electron flux are obtained from an integral equation, which determines the best relationship between the 427.8-nm intensity height profile and an arbitrary particle energy spectrum. A dimensionless function of the energy dissipation is used as the core in the integral equation. The estimated average energy of electron flux, which generated the isolated diffuse arc, is 1–2 keV higher in the central part of the arc in comparison to values at its borders. Text kola peninsula Copernicus Publications: E-Journals Kola Peninsula Annales Geophysicae 25 5 1131 1139
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In this paper we study the spatial distribution of optical volume emission rates and peculiarities of the luminosity intensity within weak diffuse auroral arcs recovered by means of auroral tomography. The tomographic images are obtained from sets of scanning multi-channel photometer data obtained in February 1999 on the Kola Peninsula in Russia at three sites of a chain extending 226 km along the geomagnetic meridian. The 427.8- and 557.7-nm emissions of a 15-s time resolution observed within one hour during low geomagnetic activity are analyzed. We found that the intensity profile of an individual arc along the geomagnetic meridian has an inverted-V-shape. The luminosity maximum altitude decrease by 4–14 km at about 140 km distance in the south-north direction can be observed during two or more diffuse arcs. The parameters of the precipitating electron flux are obtained from an integral equation, which determines the best relationship between the 427.8-nm intensity height profile and an arbitrary particle energy spectrum. A dimensionless function of the energy dissipation is used as the core in the integral equation. The estimated average energy of electron flux, which generated the isolated diffuse arc, is 1–2 keV higher in the central part of the arc in comparison to values at its borders.
format Text
author Dashkevich, Zh. V.
Ivanov, V. E.
Khudukon, B. Z.
spellingShingle Dashkevich, Zh. V.
Ivanov, V. E.
Khudukon, B. Z.
Features of stable diffuse arcs observed by means of auroral tomography
author_facet Dashkevich, Zh. V.
Ivanov, V. E.
Khudukon, B. Z.
author_sort Dashkevich, Zh. V.
title Features of stable diffuse arcs observed by means of auroral tomography
title_short Features of stable diffuse arcs observed by means of auroral tomography
title_full Features of stable diffuse arcs observed by means of auroral tomography
title_fullStr Features of stable diffuse arcs observed by means of auroral tomography
title_full_unstemmed Features of stable diffuse arcs observed by means of auroral tomography
title_sort features of stable diffuse arcs observed by means of auroral tomography
publishDate 2018
url https://doi.org/10.5194/angeo-25-1131-2007
https://angeo.copernicus.org/articles/25/1131/2007/
geographic Kola Peninsula
geographic_facet Kola Peninsula
genre kola peninsula
genre_facet kola peninsula
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-25-1131-2007
https://angeo.copernicus.org/articles/25/1131/2007/
op_doi https://doi.org/10.5194/angeo-25-1131-2007
container_title Annales Geophysicae
container_volume 25
container_issue 5
container_start_page 1131
op_container_end_page 1139
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