Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms
P(論文) The phase and the field strength of 12.1kHz Omega signals propagating from Aldra, Norway have been continuously recorded at three stations (Tjornes, Isafjordur and Husafell) in Iceland using a phase locked receiver with a loop antenna parallel to the great circle path between Aldra and each st...
Main Authors: | , , , |
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Language: | English |
Published: |
1987
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/record/2157/files/KJ00000012710.pdf https://nipr.repo.nii.ac.jp/records/2157 |
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author | Araki, Takashi Sato, Natsuo Fujii, Ryoichi Kikuchi, Takashi |
author_facet | Araki, Takashi Sato, Natsuo Fujii, Ryoichi Kikuchi, Takashi |
author_sort | Araki, Takashi |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) The phase and the field strength of 12.1kHz Omega signals propagating from Aldra, Norway have been continuously recorded at three stations (Tjornes, Isafjordur and Husafell) in Iceland using a phase locked receiver with a loop antenna parallel to the great circle path between Aldra and each stations. Sudden phase and amplitude changes associated with magnetic substorms were observed on the VLF signals, for which the phase was advanced and amplitude was increased. From the results of calculation using the full wave method with a sharp density gradient model, it is suggested that these anomalies may be interpreted to be caused by precipitating high energetic electrons. That is, the density gradient in the lower ionosphere becomes steep, and the VLF signal intensity increases due to reflection at the sharp boundary. It is also suggested from the differences of the onset time of the phase and amplitude anomaly observed at the three stations that the particle precipitation region was restricted in a small area. departmental bulletin paper |
genre | Iceland Memoirs of National Institute of Polar Research Polar Research |
genre_facet | Iceland Memoirs of National Institute of Polar Research Polar Research |
geographic | Aldra Husafell Norway |
geographic_facet | Aldra Husafell Norway |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002157 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(13.100,13.100,66.400,66.400) ENVELOPE(-20.893,-20.893,64.700,64.700) |
op_collection_id | ftnipr |
op_relation | Memoirs of National Institute of Polar Research. Special issue 47 109 116 AA00733561 https://nipr.repo.nii.ac.jp/record/2157/files/KJ00000012710.pdf https://nipr.repo.nii.ac.jp/records/2157 |
publishDate | 1987 |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002157 2025-04-13T14:21:13+00:00 Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms Araki, Takashi Sato, Natsuo Fujii, Ryoichi Kikuchi, Takashi 1987-03 application/pdf https://nipr.repo.nii.ac.jp/record/2157/files/KJ00000012710.pdf https://nipr.repo.nii.ac.jp/records/2157 eng eng Memoirs of National Institute of Polar Research. Special issue 47 109 116 AA00733561 https://nipr.repo.nii.ac.jp/record/2157/files/KJ00000012710.pdf https://nipr.repo.nii.ac.jp/records/2157 1987 ftnipr 2025-03-19T10:19:56Z P(論文) The phase and the field strength of 12.1kHz Omega signals propagating from Aldra, Norway have been continuously recorded at three stations (Tjornes, Isafjordur and Husafell) in Iceland using a phase locked receiver with a loop antenna parallel to the great circle path between Aldra and each stations. Sudden phase and amplitude changes associated with magnetic substorms were observed on the VLF signals, for which the phase was advanced and amplitude was increased. From the results of calculation using the full wave method with a sharp density gradient model, it is suggested that these anomalies may be interpreted to be caused by precipitating high energetic electrons. That is, the density gradient in the lower ionosphere becomes steep, and the VLF signal intensity increases due to reflection at the sharp boundary. It is also suggested from the differences of the onset time of the phase and amplitude anomaly observed at the three stations that the particle precipitation region was restricted in a small area. departmental bulletin paper Other/Unknown Material Iceland Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Aldra ENVELOPE(13.100,13.100,66.400,66.400) Husafell ENVELOPE(-20.893,-20.893,64.700,64.700) Norway |
spellingShingle | Araki, Takashi Sato, Natsuo Fujii, Ryoichi Kikuchi, Takashi Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title | Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title_full | Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title_fullStr | Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title_full_unstemmed | Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title_short | Phase and amplitude of VLF Omega signals observed simultaneously at three stations in Iceland in association with magnetospheric substorms |
title_sort | phase and amplitude of vlf omega signals observed simultaneously at three stations in iceland in association with magnetospheric substorms |
url | https://nipr.repo.nii.ac.jp/record/2157/files/KJ00000012710.pdf https://nipr.repo.nii.ac.jp/records/2157 |