Diurnal variation of atmospheric electric field at the summit of Mount Fuji, Japan, distinctly different from the Carnegie curve in the summertime

Author:

Kamogawa Masashi1,Suzuki Yuko1,Sakai Rikuma1,Fujiwara Hironobu2,Torii Tatsuo3,Kakinami Yoshihiro4ORCID,Watanabe Yasuyuki1,Sato Ryoe1,Hashimoto Satoshi1,Okochi Hiroshi5,Miura Kazuhiko6,Yasuda Hiroshi7,Orihara Yoshiaki1,Suzuki Tomoyuki1

Affiliation:

1. Department of Physics; Tokyo Gakugei University; Tokyo Japan

2. JSG High School; Tokyo Japan

3. Japan Atomic Energy Agency; Tokyo Japan

4. School of Systems Engineering; Kochi University of Technology; Kochi Japan

5. Faculty of Science and Engineering; Waseda University; Tokyo Japan

6. Faculty of Science; Tokyo University of Science; Tokyo Japan

7. National Institute of Radiological Sciences; Chiba Japan

Funder

Ministry of Education, Science, Sports and Culture

Scientific Research (B)

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference12 articles.

1. The atmospheric electric climate at Mauna Loa Observatory, Hawaii;Cobb;J. Atmos. Sci.,1968

2. Air-Earth current measurements at Kew, London, 1909-1979;Harrison;Atmos. Res.,2005

3. Present state of research on atmospheric electricity;Imyanitov;Sov. Phys. Usp.,1962

4. Sea of cloud observed from Mt. Fuji and its volume [in Japanese];Ishida;Tenki,1957

5. The diurnal variation of atmospheric electricity as a meteorological-aerological phenomenon;Israël;J. Meteorol.,1952

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