REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966

The observation of geomagnetic micropulsations with period from 300 to 0.5 seconds has been carried out by the JARE wintering party at Syowa Station from April, 1966. Geomagnetic signals are registered on a paper chart and a magnetic tape, using a slow speed tape recorder. In this report, characteri...

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Main Author: Susumu KOKUBUN
Format: Article
Language:English
Published: National Institute of Polar Research 1963-03-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00007502
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author Susumu KOKUBUN
author_facet Susumu KOKUBUN
author_sort Susumu KOKUBUN
collection DOAJ
description The observation of geomagnetic micropulsations with period from 300 to 0.5 seconds has been carried out by the JARE wintering party at Syowa Station from April, 1966. Geomagnetic signals are registered on a paper chart and a magnetic tape, using a slow speed tape recorder. In this report, characteristics of the recording system are briefly described and the preliminary results mainly for micropulsations of the pc-1 category, observed in 1966, are presented. Pc-1 pulsations are predominantly observed in the daytime at Syowa Station, and about one half of micropulsations with frequency of 0.2-2 Hz show a recurrent structure in f-t display. It is found that pc-1 pulsations are often associated with sudden commencements of magnetic storms which occur around local noon, and that most of ssc pulsations do not have a recurrent structure, although rising frequency of structural elements is noted in f-t display. Some spectral characteristics of pi and pc-2, 3 are also discussed.
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spelling doaj.art-1a74916524a149f69f61c4e4527cc7342022-12-21T18:57:04ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1963-03-013111110.15094/00007502REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966Susumu KOKUBUN0Geophysical Laboratory, Faculty of Science, University of TokyoThe observation of geomagnetic micropulsations with period from 300 to 0.5 seconds has been carried out by the JARE wintering party at Syowa Station from April, 1966. Geomagnetic signals are registered on a paper chart and a magnetic tape, using a slow speed tape recorder. In this report, characteristics of the recording system are briefly described and the preliminary results mainly for micropulsations of the pc-1 category, observed in 1966, are presented. Pc-1 pulsations are predominantly observed in the daytime at Syowa Station, and about one half of micropulsations with frequency of 0.2-2 Hz show a recurrent structure in f-t display. It is found that pc-1 pulsations are often associated with sudden commencements of magnetic storms which occur around local noon, and that most of ssc pulsations do not have a recurrent structure, although rising frequency of structural elements is noted in f-t display. Some spectral characteristics of pi and pc-2, 3 are also discussed.http://doi.org/10.15094/00007502
spellingShingle Susumu KOKUBUN
REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
Antarctic Record
title REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
title_full REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
title_fullStr REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
title_full_unstemmed REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
title_short REPORT ON OBSERVATION OF GEOMAGNETIC MICROPULSATIONS AT SYOWA STATION IN 1966
title_sort report on observation of geomagnetic micropulsations at syowa station in 1966
url http://doi.org/10.15094/00007502
work_keys_str_mv AT susumukokubun reportonobservationofgeomagneticmicropulsationsatsyowastationin1966