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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 空電研究所報告
  4. 8(1-2)

極年観測における空電強度記録について

http://hdl.handle.net/2237/21750
http://hdl.handle.net/2237/21750
2590ad62-d84d-4b51-ba40-0ed54b558af8
名前 / ファイル ライセンス アクション
bulria_8_1-2_26.pdf bulria_8_1-2_26.pdf (991.9 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2015-04-28
タイトル
タイトル 極年観測における空電強度記録について
言語 ja
その他のタイトル
その他のタイトル ON FIELD INTENSITY RECORDING OF ATMOSPHERICS AT 27 kc/s IN ACOORDANCE WITH THE RECOMMENDATION OF WMO
言語 en
著者 金原, 淳

× 金原, 淳

WEKO 57583

ja 金原, 淳

Search repository
木村, 靖子

× 木村, 靖子

WEKO 57584

ja 木村, 靖子

Search repository
KIMPARA, Atsushi

× KIMPARA, Atsushi

WEKO 57585

en KIMPARA, Atsushi

Search repository
KIMURA, Yasuko

× KIMURA, Yasuko

WEKO 57586

en KIMURA, Yasuko

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
抄録
内容記述 In order to see if the recommendation 40 of working group of WMO in 1957 can be applied well on the results obtained in Japan, the authors examined the records of intensity meters of atmospherics at 27 kc/s observed continuosly in 1957 at Toyokawa station. They found fairly regular behaviours of atmospherics which can be reasonably explained by the distribution of sources with seasonal variations as well as by the principle of wave propagation. "A" (Sunrise effect) is found generally 20 min. before sunrise except in winter where it is found about 2 hours before sunrise. "B" (First minimum) and "C" (Recovery effect) are often found more than once and also found frequently in the evening. "D" (Morning minimum) is found about 2 hours after sunrise, but sometimes not c1early. "E" (Afternoon maximum) is found about 2 hours before sunset and sometimes indicates flat maximum. "F" (Late minimum) is found within half-hour about sunset. "G" (Night maximum) is not found in Toyokawa. After sunset the field intensity of atmospherics increases gradually and reaches night levels abeut 2½ hours after sunset, and keeps its level nearly constant till dawn when "A" is found. "G" should be called sunset effect in Japan. It is due to the difference of distribution of sources between Europe and Asia.
言語 en
内容記述タイプ Abstract
出版者
言語 ja
出版者 名古屋大学空電研究所
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0465-7756
書誌情報 ja : 空電研究所報告

巻 8, 号 1-2, p. 26-32, 発行日 1958-03-20
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/21750
識別子タイプ HDL
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