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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. Proceedings of the Research Institute of Atmospherics, Nagoya University
  4. 5

ON FIELD ITENSITY RECORDING OF ATMOSPHERICS AT 27 kc/s IN ACCORDANCE WITH THE RECOMMENDATION OF WMO

http://hdl.handle.net/2237/21631
http://hdl.handle.net/2237/21631
0fa60bba-db74-4488-84a0-657f83ab386b
名前 / ファイル ライセンス アクション
Vol5-3.pdf Vol5-3.pdf (1.2 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2015-04-20
タイトル
タイトル ON FIELD ITENSITY RECORDING OF ATMOSPHERICS AT 27 kc/s IN ACCORDANCE WITH THE RECOMMENDATION OF WMO
言語 en
著者 KIMPARA, ATSUSHI

× KIMPARA, ATSUSHI

WEKO 57191

en KIMPARA, ATSUSHI

Search repository
KIMURA, YASUKO

× KIMURA, YASUKO

WEKO 57192

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 ks/s observed continuously 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 clearly. "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 about 2 1/2 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 en
出版者 The Research Institute of Atmospherics, Nagoya University
言語
言語 eng
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 0077-264X
書誌情報 en : Proceedings of the Research Institute of Atmospherics, Nagoya University

巻 5, p. 21-29, 発行日 1958-03-25
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/21631
識別子タイプ HDL
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