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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/2237/216310fa60bba-db74-4488-84a0-657f83ab386b
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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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× KIMURA, YASUKO |
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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 |
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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 |