VLF HISS AT SYOWA STATION, ANTARCTICA

1970-03-30 Analyzing the VLF hiss (or auroral hiss) record at Syowa Station (geomagnetic latitude -69.7°) , Antarctica, which induced the observation on polarization, incident angle and intensity, we have found the evidence that VLF hiss is right-handed, and elliptically polarized, wave (whistler mo...

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Main Authors: TANAKA, Yoshihito, 59017, NISHINO, Masanori, 59018, IWAI, Akira, 59019
Language:English
Published: The Research Institute of Atmospherics, Nagoya University 1970
Subjects:
Online Access:http://hdl.handle.net/2237/22119
id ftnagoyauniv:oai:nagoya.repo.nii.ac.jp:00020205
record_format openpolar
spelling ftnagoyauniv:oai:nagoya.repo.nii.ac.jp:00020205 2023-05-15T14:02:41+02:00 VLF HISS AT SYOWA STATION, ANTARCTICA TANAKA, Yoshihito 59017 NISHINO, Masanori 59018 IWAI, Akira 59019 1970-03-30 http://hdl.handle.net/2237/22119 eng eng The Research Institute of Atmospherics, Nagoya University Proceedings of the Research Institute of Atmospherics, Nagoya University 17 43 55 http://hdl.handle.net/2237/22119 0077-264X 1970 ftnagoyauniv 2023-02-20T14:30:35Z 1970-03-30 Analyzing the VLF hiss (or auroral hiss) record at Syowa Station (geomagnetic latitude -69.7°) , Antarctica, which induced the observation on polarization, incident angle and intensity, we have found the evidence that VLF hiss is right-handed, and elliptically polarized, wave (whistler mode wave) , and its incident angle into free space below the ionosphere is small. We have also found that the upper frequency of VLF hiss which appear in advance of the break-up of over-head aurora reaches more than 100KHz and that the maximum energy of the spectrum is received at a frequency near to 10 KHz. Further it is suggested that VLF hiss in the auroral zone is generated by Cerenkov radiation process in the low altitude dark magnetosphere, and that it does not propagate to the middle and low latitudes. departmental bulletin paper Other/Unknown Material Antarc* Antarctica Nagoya University: NAGOYA Repository Syowa Station
institution Open Polar
collection Nagoya University: NAGOYA Repository
op_collection_id ftnagoyauniv
language English
description 1970-03-30 Analyzing the VLF hiss (or auroral hiss) record at Syowa Station (geomagnetic latitude -69.7°) , Antarctica, which induced the observation on polarization, incident angle and intensity, we have found the evidence that VLF hiss is right-handed, and elliptically polarized, wave (whistler mode wave) , and its incident angle into free space below the ionosphere is small. We have also found that the upper frequency of VLF hiss which appear in advance of the break-up of over-head aurora reaches more than 100KHz and that the maximum energy of the spectrum is received at a frequency near to 10 KHz. Further it is suggested that VLF hiss in the auroral zone is generated by Cerenkov radiation process in the low altitude dark magnetosphere, and that it does not propagate to the middle and low latitudes. departmental bulletin paper
author TANAKA, Yoshihito
59017
NISHINO, Masanori
59018
IWAI, Akira
59019
spellingShingle TANAKA, Yoshihito
59017
NISHINO, Masanori
59018
IWAI, Akira
59019
VLF HISS AT SYOWA STATION, ANTARCTICA
author_facet TANAKA, Yoshihito
59017
NISHINO, Masanori
59018
IWAI, Akira
59019
author_sort TANAKA, Yoshihito
title VLF HISS AT SYOWA STATION, ANTARCTICA
title_short VLF HISS AT SYOWA STATION, ANTARCTICA
title_full VLF HISS AT SYOWA STATION, ANTARCTICA
title_fullStr VLF HISS AT SYOWA STATION, ANTARCTICA
title_full_unstemmed VLF HISS AT SYOWA STATION, ANTARCTICA
title_sort vlf hiss at syowa station, antarctica
publisher The Research Institute of Atmospherics, Nagoya University
publishDate 1970
url http://hdl.handle.net/2237/22119
geographic Syowa Station
geographic_facet Syowa Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation Proceedings of the Research Institute of Atmospherics, Nagoya University
17
43
55
http://hdl.handle.net/2237/22119
0077-264X
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