Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)

VLF emissions were observed at Syowa Station by the 11th wintering party of the Japanese Antarctic Research Expedition in 1970-1971. The present paper deals particularly with the records of auroral hiss emissions, which are believed to be emitted by precipitating electrons in the aurora. It is shown...

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Bibliographic Details
Main Authors: Kazuo MAKITA, Hiroshi FUKUNISHI
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1973
Subjects:
geo
Online Access:https://doi.org/10.15094/00007699
https://doaj.org/article/c667ae7d402140f89ec39ff95d04a588
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:c667ae7d402140f89ec39ff95d04a588 2023-05-15T14:04:00+02:00 Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition) Kazuo MAKITA Hiroshi FUKUNISHI 1973-03-01 https://doi.org/10.15094/00007699 https://doaj.org/article/c667ae7d402140f89ec39ff95d04a588 en other eng National Institute of Polar Research doi:10.15094/00007699 0085-7289 2432-079X https://doaj.org/article/c667ae7d402140f89ec39ff95d04a588 undefined Antarctic Record, Iss 46, Pp 1-15 (1973) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1973 fttriple https://doi.org/10.15094/00007699 2023-01-22T19:13:54Z VLF emissions were observed at Syowa Station by the 11th wintering party of the Japanese Antarctic Research Expedition in 1970-1971. The present paper deals particularly with the records of auroral hiss emissions, which are believed to be emitted by precipitating electrons in the aurora. It is shown that the power spectrum of the hiss emissions is confined in the low-frequency range between 4-32kHz if the auroral arcs lie near the poleward horizon of Syowa Station, while it is extended to frequencies as high as 128kHz if the active auroral arcs appear near the zenith. This can be explained by differences in the height of the emission region and in the propagation path of the hiss in the ionosphere : the high-frequency (~64kHz) hiss is emitted at low altitudes of 1000-1500km, its propagation path being limited to a narrow region near the location of the auroral arcs, while the low-frequency (~8kHz) hiss is emitted at higher altitudes of 3000-3500km, its propagation path spreading widely due to the refraction effect in the ionosphere. Article in Journal/Newspaper Antarc* Antarctic Unknown Antarctic Syowa Station
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Kazuo MAKITA
Hiroshi FUKUNISHI
Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
topic_facet geo
description VLF emissions were observed at Syowa Station by the 11th wintering party of the Japanese Antarctic Research Expedition in 1970-1971. The present paper deals particularly with the records of auroral hiss emissions, which are believed to be emitted by precipitating electrons in the aurora. It is shown that the power spectrum of the hiss emissions is confined in the low-frequency range between 4-32kHz if the auroral arcs lie near the poleward horizon of Syowa Station, while it is extended to frequencies as high as 128kHz if the active auroral arcs appear near the zenith. This can be explained by differences in the height of the emission region and in the propagation path of the hiss in the ionosphere : the high-frequency (~64kHz) hiss is emitted at low altitudes of 1000-1500km, its propagation path being limited to a narrow region near the location of the auroral arcs, while the low-frequency (~8kHz) hiss is emitted at higher altitudes of 3000-3500km, its propagation path spreading widely due to the refraction effect in the ionosphere.
format Article in Journal/Newspaper
author Kazuo MAKITA
Hiroshi FUKUNISHI
author_facet Kazuo MAKITA
Hiroshi FUKUNISHI
author_sort Kazuo MAKITA
title Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
title_short Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
title_full Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
title_fullStr Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
title_full_unstemmed Observation of VLF Emissions at Syowa Station in 1970-1971 : I. Relationship between the Occurrence of Auroral Hiss Emissions and the Location of Auroral Arcs (Reports of the Japanese Antarctic Research Expedition)
title_sort observation of vlf emissions at syowa station in 1970-1971 : i. relationship between the occurrence of auroral hiss emissions and the location of auroral arcs (reports of the japanese antarctic research expedition)
publisher National Institute of Polar Research
publishDate 1973
url https://doi.org/10.15094/00007699
https://doaj.org/article/c667ae7d402140f89ec39ff95d04a588
geographic Antarctic
Syowa Station
geographic_facet Antarctic
Syowa Station
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Antarctic Record, Iss 46, Pp 1-15 (1973)
op_relation doi:10.15094/00007699
0085-7289
2432-079X
https://doaj.org/article/c667ae7d402140f89ec39ff95d04a588
op_rights undefined
op_doi https://doi.org/10.15094/00007699
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