Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions

Average energy and total energy flux of the incident electrons in active auroras are estimated by using the intensity ratio of auroral emissions measured with a multi-channel photometer at Syowa Station, Antarctica, in 1990. To avoid possible ambiguities which are mainly caused by quenching effects...

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Bibliographic Details
Main Authors: Takayuki Ono, Ryusuke Satake, Takeo Yoshino, Takeo Hirasawa
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1992
Subjects:
geo
Online Access:https://doi.org/10.15094/00008764
https://doaj.org/article/6ae642e8b3b64b2383cb833642282b78
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:6ae642e8b3b64b2383cb833642282b78 2023-05-15T14:04:55+02:00 Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions Takayuki Ono Ryusuke Satake Takeo Yoshino Takeo Hirasawa 1992-07-01 https://doi.org/10.15094/00008764 https://doaj.org/article/6ae642e8b3b64b2383cb833642282b78 en other eng National Institute of Polar Research doi:10.15094/00008764 0085-7289 2432-079X https://doaj.org/article/6ae642e8b3b64b2383cb833642282b78 undefined Antarctic Record, Vol 36, Iss 2, Pp 163-180 (1992) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1992 fttriple https://doi.org/10.15094/00008764 2023-01-22T19:12:19Z Average energy and total energy flux of the incident electrons in active auroras are estimated by using the intensity ratio of auroral emissions measured with a multi-channel photometer at Syowa Station, Antarctica, in 1990. To avoid possible ambiguities which are mainly caused by quenching effects on meta-stable species and complex excitation processes, we used intensity ratios of the emissions of allowed transitions such as 844.6nm (OI), 670.5nm (N_21PG), and 427.8nm (N_2^+1NG). Measured intensity ratios were directly compared with a result of model calculation of auroral emissions. The estimated energy parameters in active auroras showed a rapid change of average energy as well as total energy flux of electrons associated with pulsating auroras and intense auroral arcs. Average energy and total energy flux of the auroral electrons determined by the present method were consistent with the result of the previous in-situ observations of precipitating electrons. Our data analyses on active arcs in break-up phase showed that usage of the 427.8nm emission has difficulty due to a scattering effect of the atmosphere. Usage of 670.5nm emission in place of 427.8nm made it possible to evaluate the energy parameters of electrons even in the vicinity of intense auroral arcs. Article in Journal/Newspaper Antarc* Antarctica Unknown Syowa Station
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Takayuki Ono
Ryusuke Satake
Takeo Yoshino
Takeo Hirasawa
Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
topic_facet geo
description Average energy and total energy flux of the incident electrons in active auroras are estimated by using the intensity ratio of auroral emissions measured with a multi-channel photometer at Syowa Station, Antarctica, in 1990. To avoid possible ambiguities which are mainly caused by quenching effects on meta-stable species and complex excitation processes, we used intensity ratios of the emissions of allowed transitions such as 844.6nm (OI), 670.5nm (N_21PG), and 427.8nm (N_2^+1NG). Measured intensity ratios were directly compared with a result of model calculation of auroral emissions. The estimated energy parameters in active auroras showed a rapid change of average energy as well as total energy flux of electrons associated with pulsating auroras and intense auroral arcs. Average energy and total energy flux of the auroral electrons determined by the present method were consistent with the result of the previous in-situ observations of precipitating electrons. Our data analyses on active arcs in break-up phase showed that usage of the 427.8nm emission has difficulty due to a scattering effect of the atmosphere. Usage of 670.5nm emission in place of 427.8nm made it possible to evaluate the energy parameters of electrons even in the vicinity of intense auroral arcs.
format Article in Journal/Newspaper
author Takayuki Ono
Ryusuke Satake
Takeo Yoshino
Takeo Hirasawa
author_facet Takayuki Ono
Ryusuke Satake
Takeo Yoshino
Takeo Hirasawa
author_sort Takayuki Ono
title Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
title_short Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
title_full Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
title_fullStr Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
title_full_unstemmed Energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
title_sort energy parameters of the incident auroral electrons derived by the intensity ratio of auroral emissions
publisher National Institute of Polar Research
publishDate 1992
url https://doi.org/10.15094/00008764
https://doaj.org/article/6ae642e8b3b64b2383cb833642282b78
geographic Syowa Station
geographic_facet Syowa Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Antarctic Record, Vol 36, Iss 2, Pp 163-180 (1992)
op_relation doi:10.15094/00008764
0085-7289
2432-079X
https://doaj.org/article/6ae642e8b3b64b2383cb833642282b78
op_rights undefined
op_doi https://doi.org/10.15094/00008764
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