Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1

P(論文) The broadband whistler-mode (w-mode) emissions in LF/MF bands observed at low altitudes in the nighttime auroral zone are examined in detail, especially from the viewpoint of the spectral characteristics and directions of wave vectors of the emissions using the ISIS-1 data including the fixed...

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Main Authors: Aikyo, Kazuhiro, Ondoh, Tadanori, Ohtaka, Kazuhiro
Language:English
Published: National Institute of Polar Research 1988
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/4046/files/KJ00000035892.pdf
https://doi.org/10.15094/00004046
https://nipr.repo.nii.ac.jp/records/4046
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author Aikyo, Kazuhiro
Ondoh, Tadanori
Ohtaka, Kazuhiro
author_facet Aikyo, Kazuhiro
Ondoh, Tadanori
Ohtaka, Kazuhiro
author_sort Aikyo, Kazuhiro
collection National Institute of Polar Research Repository, Japan
description P(論文) The broadband whistler-mode (w-mode) emissions in LF/MF bands observed at low altitudes in the nighttime auroral zone are examined in detail, especially from the viewpoint of the spectral characteristics and directions of wave vectors of the emissions using the ISIS-1 data including the fixed and swept frequency ionograms and AGC voltage traces of the sounder receiver. The emissions are characterized by spectra with relatively sharp upper cutoff ranging 0.75 to 0.4f_H (f_H : electron gyrofrequency) and with lower frequency cutoff less than 0.1 MHz (the lowest frequency of the sounder) for many cases. The directions of wave vectors at the satellite are determined from the antenna orientation at the instant when the emissions exhibit intensity minima on AGC voltage traces in the fixed frequency mode. The resultant directions of wave vectors are used as initial conditions for ray tracing to locate the source regions and to know the directions of wave vectors at the source region. It is shown that the cyclotron maser instability driven by auroral electron with upward loss cone at low altitudes is the most probable source mechanism which explains some characteristics of the observed emissions, particularly, of their high frequency portion. departmental bulletin paper
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
id ftnipr:oai:nipr.repo.nii.ac.jp:00004046
institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00004046
op_relation Proceedings of the NIPR Symposium on Upper Atmosphere Physics
1
173
184
AA10756224
https://nipr.repo.nii.ac.jp/record/4046/files/KJ00000035892.pdf
https://doi.org/10.15094/00004046
https://nipr.repo.nii.ac.jp/records/4046
publishDate 1988
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00004046 2025-04-13T14:08:17+00:00 Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1 Aikyo, Kazuhiro Ondoh, Tadanori Ohtaka, Kazuhiro 1988-02 application/pdf https://nipr.repo.nii.ac.jp/record/4046/files/KJ00000035892.pdf https://doi.org/10.15094/00004046 https://nipr.repo.nii.ac.jp/records/4046 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Upper Atmosphere Physics 1 173 184 AA10756224 https://nipr.repo.nii.ac.jp/record/4046/files/KJ00000035892.pdf https://doi.org/10.15094/00004046 https://nipr.repo.nii.ac.jp/records/4046 1988 ftnipr https://doi.org/10.15094/00004046 2025-03-19T10:19:57Z P(論文) The broadband whistler-mode (w-mode) emissions in LF/MF bands observed at low altitudes in the nighttime auroral zone are examined in detail, especially from the viewpoint of the spectral characteristics and directions of wave vectors of the emissions using the ISIS-1 data including the fixed and swept frequency ionograms and AGC voltage traces of the sounder receiver. The emissions are characterized by spectra with relatively sharp upper cutoff ranging 0.75 to 0.4f_H (f_H : electron gyrofrequency) and with lower frequency cutoff less than 0.1 MHz (the lowest frequency of the sounder) for many cases. The directions of wave vectors at the satellite are determined from the antenna orientation at the instant when the emissions exhibit intensity minima on AGC voltage traces in the fixed frequency mode. The resultant directions of wave vectors are used as initial conditions for ray tracing to locate the source regions and to know the directions of wave vectors at the source region. It is shown that the cyclotron maser instability driven by auroral electron with upward loss cone at low altitudes is the most probable source mechanism which explains some characteristics of the observed emissions, particularly, of their high frequency portion. departmental bulletin paper Other/Unknown Material Antarc* Antarctic National Institute of Polar Research Repository, Japan Antarctic The Antarctic
spellingShingle Aikyo, Kazuhiro
Ondoh, Tadanori
Ohtaka, Kazuhiro
Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title_full Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title_fullStr Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title_full_unstemmed Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title_short Some characteristics and propagation of whistler-mode LF/MF emissions as observed at low altitudes above the Antarctic region with ISIS-1
title_sort some characteristics and propagation of whistler-mode lf/mf emissions as observed at low altitudes above the antarctic region with isis-1
url https://nipr.repo.nii.ac.jp/record/4046/files/KJ00000035892.pdf
https://doi.org/10.15094/00004046
https://nipr.repo.nii.ac.jp/records/4046