Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism

The relations between average energy and total energy flux of incident electrons are examined for three types of auroras, namely, type A aurora, pulsating aurora, and discrete aurora in auroral break up. The energy parameters of primary electrons are derived by using measured intensities at 844.6nm...

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Main Authors: Kei Morishima, Takayuki Ono, Kanji Hayashi
Format: Article
Language:English
Published: National Institute of Polar Research 1993-11-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00008818
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spelling doaj-a12751d3fd894f838e5b8dd349540d7e2020-11-24T23:05:57ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1993-11-0137320523010.15094/00008818Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanismKei Morishima0Takayuki Ono1Kanji Hayashi2Faculty of Science, University of Tokyo National Institute of Polar ResearchFaculty of Science, University of TokyoThe relations between average energy and total energy flux of incident electrons are examined for three types of auroras, namely, type A aurora, pulsating aurora, and discrete aurora in auroral break up. The energy parameters of primary electrons are derived by using measured intensities at 844.6nm (OI) and 670.5nm (N_21PG) from a multi-channel photometer observation at Syowa Station, Antarctica, in 1990. It is shown that each auroral type has its own relationship between energy parameters of precipitating electrons. In a discrete aurora, downward electron energy flux generally varied proportionally with square of average energy. This tendency can be identified as an ohmic-like feature. This special relation is accounted for by a theory in which electrons are accelerated by a field-aligned-potential difference. We also found that in some discrete auroras, precipitating electrons did not show the ohmic-like behavior. These exceptional cases are thought to be caused by two factors. One is a geometric relation between auroral arcs and the field of view of the photometer. The other is the change of the L-E-L constant in the magnetosphere (M. FRIDMAN and J. LEMAIRE; J. Geophys. Res., 85,664,1980) due to temporal variations of plasma parameters, such as electron density and thermal energy in the source region of the auroral particles.http://doi.org/10.15094/00008818
collection DOAJ
language English
format Article
sources DOAJ
author Kei Morishima
Takayuki Ono
Kanji Hayashi
spellingShingle Kei Morishima
Takayuki Ono
Kanji Hayashi
Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
Antarctic Record
author_facet Kei Morishima
Takayuki Ono
Kanji Hayashi
author_sort Kei Morishima
title Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
title_short Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
title_full Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
title_fullStr Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
title_full_unstemmed Evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
title_sort evaluation of energy parameters of auroral electrons by using photometric observations and its application to investigate a generation mechanism
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1993-11-01
description The relations between average energy and total energy flux of incident electrons are examined for three types of auroras, namely, type A aurora, pulsating aurora, and discrete aurora in auroral break up. The energy parameters of primary electrons are derived by using measured intensities at 844.6nm (OI) and 670.5nm (N_21PG) from a multi-channel photometer observation at Syowa Station, Antarctica, in 1990. It is shown that each auroral type has its own relationship between energy parameters of precipitating electrons. In a discrete aurora, downward electron energy flux generally varied proportionally with square of average energy. This tendency can be identified as an ohmic-like feature. This special relation is accounted for by a theory in which electrons are accelerated by a field-aligned-potential difference. We also found that in some discrete auroras, precipitating electrons did not show the ohmic-like behavior. These exceptional cases are thought to be caused by two factors. One is a geometric relation between auroral arcs and the field of view of the photometer. The other is the change of the L-E-L constant in the magnetosphere (M. FRIDMAN and J. LEMAIRE; J. Geophys. Res., 85,664,1980) due to temporal variations of plasma parameters, such as electron density and thermal energy in the source region of the auroral particles.
url http://doi.org/10.15094/00008818
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AT takayukiono evaluationofenergyparametersofauroralelectronsbyusingphotometricobservationsanditsapplicationtoinvestigateagenerationmechanism
AT kanjihayashi evaluationofenergyparametersofauroralelectronsbyusingphotometricobservationsanditsapplicationtoinvestigateagenerationmechanism
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