ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク

P(論文) The fourth cosmic ray latitude survey in nucleonic and meson components was carried out on M/S "SOYA" during the full voyage to and from Antarctica. The observation room was the same as in the preceding survey. The intensity of the nucleonic component was measured by the same apparat...

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Main Authors: 牧野, 忠男, マキノ, タダオ, MAKINO, Tadao
Language:Japanese
Published: 国立極地研究所 1962
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/7146/files/KJ00002476068.pdf
https://doi.org/10.15094/00007146
https://nipr.repo.nii.ac.jp/records/7146
_version_ 1829308668588326912
author 牧野, 忠男
マキノ, タダオ
MAKINO, Tadao
author_facet 牧野, 忠男
マキノ, タダオ
MAKINO, Tadao
author_sort 牧野, 忠男
collection National Institute of Polar Research Repository, Japan
description P(論文) The fourth cosmic ray latitude survey in nucleonic and meson components was carried out on M/S "SOYA" during the full voyage to and from Antarctica. The observation room was the same as in the preceding survey. The intensity of the nucleonic component was measured by the same apparatus as before, while the intensity of meson component was observed by a Neher-type ionization chamber. The obtained data were corrected for barometric pressure effect and for the primary cosmic ray intensity variation deduced from the nucleonic component at sea level. The data of meson component were also corrected for atmospheric temperature effect, as well as for the above two effects. Results: 1. Obtained latitude factors were 55% for nucleonic component and 11% for meson component, respectively. 2. Knee of the latitude curves was found to be at geomagnetic latitude 35°S, and geographic longitude 20°E in both components. 3. Minimum intensity point was found to occur at geomagnetic latitude 5°S, and geographic longitude 107°E. 4. Longitude effects between 87°E-109°E and 18°E-34°E were -1.1%/deg. and -2.3%/deg., respectively in nucleonic component. The results 2, 3 and 4 were identical with those of the preceding three surveys. That is to say, they do not correspond to the relative sun spot numbers. According to the previous report the latitude factor follows the relative sun spot numbers inversely with a half year delay. Comparing with the preceding three surveys, the present result (Result 1) would be expected to become larger than 60%. However, the present result showed 55%. Also meson component in the first survey got latitude factor of 12%, so in the present survey it was expected to becomelarger than 12%, but the present result showed 11%. Therefore our result is not consistent with the preceding report. Reexamining the preceding three surveys, we have got the results shown in Fig. 2. These results mean that latitude factor rather follows the relative sun spot numbers. The results will be checked again with our next ...
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
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institution Open Polar
language Japanese
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00007146
op_relation 南極資料
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https://nipr.repo.nii.ac.jp/record/7146/files/KJ00002476068.pdf
https://doi.org/10.15094/00007146
https://nipr.repo.nii.ac.jp/records/7146
publishDate 1962
publisher 国立極地研究所
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00007146 2025-04-13T14:07:49+00:00 ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク 第5次南極地域観測隊宇宙線部門船上観測報告 REPORT ON RESULTS OF COSMIC RAY OBSERVATIONS ON M/S "SOYA" DURING THE PERIOD FROM NOV. '60 TO MAY '61 牧野, 忠男 マキノ, タダオ MAKINO, Tadao 1962-01 application/pdf https://nipr.repo.nii.ac.jp/record/7146/files/KJ00002476068.pdf https://doi.org/10.15094/00007146 https://nipr.repo.nii.ac.jp/records/7146 jpn jpn 国立極地研究所 南極資料 14 1131 1146 AN00181831 00857289 https://nipr.repo.nii.ac.jp/record/7146/files/KJ00002476068.pdf https://doi.org/10.15094/00007146 https://nipr.repo.nii.ac.jp/records/7146 551.510.535/.537 1962 ftnipr https://doi.org/10.15094/00007146 2025-03-19T10:19:57Z P(論文) The fourth cosmic ray latitude survey in nucleonic and meson components was carried out on M/S "SOYA" during the full voyage to and from Antarctica. The observation room was the same as in the preceding survey. The intensity of the nucleonic component was measured by the same apparatus as before, while the intensity of meson component was observed by a Neher-type ionization chamber. The obtained data were corrected for barometric pressure effect and for the primary cosmic ray intensity variation deduced from the nucleonic component at sea level. The data of meson component were also corrected for atmospheric temperature effect, as well as for the above two effects. Results: 1. Obtained latitude factors were 55% for nucleonic component and 11% for meson component, respectively. 2. Knee of the latitude curves was found to be at geomagnetic latitude 35°S, and geographic longitude 20°E in both components. 3. Minimum intensity point was found to occur at geomagnetic latitude 5°S, and geographic longitude 107°E. 4. Longitude effects between 87°E-109°E and 18°E-34°E were -1.1%/deg. and -2.3%/deg., respectively in nucleonic component. The results 2, 3 and 4 were identical with those of the preceding three surveys. That is to say, they do not correspond to the relative sun spot numbers. According to the previous report the latitude factor follows the relative sun spot numbers inversely with a half year delay. Comparing with the preceding three surveys, the present result (Result 1) would be expected to become larger than 60%. However, the present result showed 55%. Also meson component in the first survey got latitude factor of 12%, so in the present survey it was expected to becomelarger than 12%, but the present result showed 11%. Therefore our result is not consistent with the preceding report. Reexamining the preceding three surveys, we have got the results shown in Fig. 2. These results mean that latitude factor rather follows the relative sun spot numbers. The results will be checked again with our next ... Other/Unknown Material Antarc* Antarctica National Institute of Polar Research Repository, Japan
spellingShingle 551.510.535/.537
牧野, 忠男
マキノ, タダオ
MAKINO, Tadao
ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title_full ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title_fullStr ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title_full_unstemmed ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title_short ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
title_sort ダイ5ジ ナンキョク チイキ カンソクタイ ウチュウセン ブモン センジョウ カンソク ホウコク
topic 551.510.535/.537
topic_facet 551.510.535/.537
url https://nipr.repo.nii.ac.jp/record/7146/files/KJ00002476068.pdf
https://doi.org/10.15094/00007146
https://nipr.repo.nii.ac.jp/records/7146