VLF-Noise in the Dayside Polar Cusp

P(論文) VLF-noise measurements at several Antarctic ground stations (Mirny, Sleightrain and Vostok) are used as diagnostic of the parameters of the solar wind particles penetrating in the polar cusp region. The observed results revealed the higher level radiation zone in the dayside polar cusp region...

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Main Authors: Golikov, Yu.V., Kleimenova, N.G., Troitskaya, V.A.
Language:English
Published: 1976
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/845/files/KJ00000011819.pdf
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00000845 2024-09-09T19:02:38+00:00 VLF-Noise in the Dayside Polar Cusp Golikov, Yu.V. Kleimenova, N.G. Troitskaya, V.A. 1976-08 application/pdf https://nipr.repo.nii.ac.jp/record/845/files/KJ00000011819.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 6 97 100 AA00733561 https://nipr.repo.nii.ac.jp/record/845/files/KJ00000011819.pdf 1976 ftnipr 2024-06-17T04:03:38Z P(論文) VLF-noise measurements at several Antarctic ground stations (Mirny, Sleightrain and Vostok) are used as diagnostic of the parameters of the solar wind particles penetrating in the polar cusp region. The observed results revealed the higher level radiation zone in the dayside polar cusp region (geomagnetic latitude ∿79°) when Kp≤3; two maxima of the daily intensity of VLF noise occur around 12 h and 18 h (local magnetic time). The coincidence in time of the VLF noise growth with soft electrons precipitation probability maxima indicates that VLF noise in the dayside polar cusp is generated by precipitating soft electrons. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic Mirny ENVELOPE(93.009,93.009,-66.553,-66.553)
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description P(論文) VLF-noise measurements at several Antarctic ground stations (Mirny, Sleightrain and Vostok) are used as diagnostic of the parameters of the solar wind particles penetrating in the polar cusp region. The observed results revealed the higher level radiation zone in the dayside polar cusp region (geomagnetic latitude ∿79°) when Kp≤3; two maxima of the daily intensity of VLF noise occur around 12 h and 18 h (local magnetic time). The coincidence in time of the VLF noise growth with soft electrons precipitation probability maxima indicates that VLF noise in the dayside polar cusp is generated by precipitating soft electrons. departmental bulletin paper
author Golikov, Yu.V.
Kleimenova, N.G.
Troitskaya, V.A.
spellingShingle Golikov, Yu.V.
Kleimenova, N.G.
Troitskaya, V.A.
VLF-Noise in the Dayside Polar Cusp
author_facet Golikov, Yu.V.
Kleimenova, N.G.
Troitskaya, V.A.
author_sort Golikov, Yu.V.
title VLF-Noise in the Dayside Polar Cusp
title_short VLF-Noise in the Dayside Polar Cusp
title_full VLF-Noise in the Dayside Polar Cusp
title_fullStr VLF-Noise in the Dayside Polar Cusp
title_full_unstemmed VLF-Noise in the Dayside Polar Cusp
title_sort vlf-noise in the dayside polar cusp
publishDate 1976
url https://nipr.repo.nii.ac.jp/record/845/files/KJ00000011819.pdf
long_lat ENVELOPE(93.009,93.009,-66.553,-66.553)
geographic Antarctic
Mirny
geographic_facet Antarctic
Mirny
genre Antarc*
Antarctic
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctic
Memoirs of National Institute of Polar Research
Polar Research
op_relation Memoirs of National Institute of Polar Research. Special issue
6
97
100
AA00733561
https://nipr.repo.nii.ac.jp/record/845/files/KJ00000011819.pdf
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