Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse

During the solar eclipse on August 11, 1961, the continuous recording of h'-f observation was made in vertical incidence at Syowa Base in Antarctica, and in spite of the period of very low solar zenith angle, it was possible to find the effect of the eclipse on the ionograms. The recordings at...

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Bibliographic Details
Main Authors: Sadao HASEGAWA, Nobuhiro KAWAJIRI
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1964
Subjects:
geo
Online Access:https://doi.org/10.15094/00007314
https://doaj.org/article/86bfccd8a3d6480d8f5d3a13546e1843
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:86bfccd8a3d6480d8f5d3a13546e1843 2023-05-15T13:42:08+02:00 Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse Sadao HASEGAWA Nobuhiro KAWAJIRI 1964-02-01 https://doi.org/10.15094/00007314 https://doaj.org/article/86bfccd8a3d6480d8f5d3a13546e1843 en other eng National Institute of Polar Research doi:10.15094/00007314 0085-7289 2432-079X https://doaj.org/article/86bfccd8a3d6480d8f5d3a13546e1843 undefined Antarctic Record, Iss 20, Pp 1688-1706 (1964) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1964 fttriple https://doi.org/10.15094/00007314 2023-01-22T19:13:41Z During the solar eclipse on August 11, 1961, the continuous recording of h'-f observation was made in vertical incidence at Syowa Base in Antarctica, and in spite of the period of very low solar zenith angle, it was possible to find the effect of the eclipse on the ionograms. The recordings at this time were obtained of only the F2 region in the ionosphere, and the variation of electron density during the solar eclipse at a certain height of the F2 region was more remarkable than the variation of the critical frequency. The results of analysis of the observations are summarized as follows: (i) Electron in the F2 region seems to decrease by the attachment process, and the order of magnitude of the attachment coefficient can be estimated at 1.5×10^ to 2.0×10^sec^ at 300km. (ii) On the assumption of the above-mentioned values as the attachment coefficient, the computed values of an electron density during the eclipse show a good agreement with the observational values up to the maximum phase of the eclipse, but beyond the maximum phase, the observational values continue to increase rapidly in electron density until after the end of eclipse. It may be suggested that the phenomena of electron increase are due to an effect such as the ionization of charged particles, (iii) In our observation, the value of scale height obtained, as the attachment process of electron to (O_2) oxygen, is about 30 km at 300 km levels of the F2 layer. Article in Journal/Newspaper Antarc* Antarctica Unknown
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Sadao HASEGAWA
Nobuhiro KAWAJIRI
Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
topic_facet geo
description During the solar eclipse on August 11, 1961, the continuous recording of h'-f observation was made in vertical incidence at Syowa Base in Antarctica, and in spite of the period of very low solar zenith angle, it was possible to find the effect of the eclipse on the ionograms. The recordings at this time were obtained of only the F2 region in the ionosphere, and the variation of electron density during the solar eclipse at a certain height of the F2 region was more remarkable than the variation of the critical frequency. The results of analysis of the observations are summarized as follows: (i) Electron in the F2 region seems to decrease by the attachment process, and the order of magnitude of the attachment coefficient can be estimated at 1.5×10^ to 2.0×10^sec^ at 300km. (ii) On the assumption of the above-mentioned values as the attachment coefficient, the computed values of an electron density during the eclipse show a good agreement with the observational values up to the maximum phase of the eclipse, but beyond the maximum phase, the observational values continue to increase rapidly in electron density until after the end of eclipse. It may be suggested that the phenomena of electron increase are due to an effect such as the ionization of charged particles, (iii) In our observation, the value of scale height obtained, as the attachment process of electron to (O_2) oxygen, is about 30 km at 300 km levels of the F2 layer.
format Article in Journal/Newspaper
author Sadao HASEGAWA
Nobuhiro KAWAJIRI
author_facet Sadao HASEGAWA
Nobuhiro KAWAJIRI
author_sort Sadao HASEGAWA
title Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
title_short Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
title_full Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
title_fullStr Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
title_full_unstemmed Results of Ionospheric Observation at Syowa Base, Antarctica, during the Solar Eclipse
title_sort results of ionospheric observation at syowa base, antarctica, during the solar eclipse
publisher National Institute of Polar Research
publishDate 1964
url https://doi.org/10.15094/00007314
https://doaj.org/article/86bfccd8a3d6480d8f5d3a13546e1843
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Antarctic Record, Iss 20, Pp 1688-1706 (1964)
op_relation doi:10.15094/00007314
0085-7289
2432-079X
https://doaj.org/article/86bfccd8a3d6480d8f5d3a13546e1843
op_rights undefined
op_doi https://doi.org/10.15094/00007314
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