Simultaneous Observations of Atmospheric Electric Field, Aerosols, and Clouds on the R/V Hakuho Maru over the Pacific Ocean
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- Kamogawa Masashi
- Department of Physics, Tokyo Gakugei University
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- Ohhara Kosei
- Department of Physics, Tokyo Gakugei University
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- Ueda Sayako
- Department of Physics, Faculty of Science, Tokyo University of Science
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- Miura Kazuhiko
- Department of Physics, Faculty of Science, Tokyo University of Science
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- Yajima Kazuaki
- National Institute of Radiological Sciences
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- Hashimoto Satoshi
- Department of Physics, Tokyo Gakugei University
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- Nakamura Maho
- Department of Physics, Tokyo Gakugei University
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- Kakinami Yoshihiro
- School of Systems Engineering, Kochi University of Technology
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- Furutani Hiroshi
- Atmosphere and Ocean Research Institute, The University of Tokyo
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- Uematsu Mitsuo
- Atmosphere and Ocean Research Institute, The University of Tokyo
抄録
There is an ionospheric potential between conductive solid-earth and ionosphere which reaches approximately 250 kV. The ionospheric potential is generated by the spherical shell capacitance of which is formed by positively charged ionosphere and negatively charged solid-earth. The capacitance is charged and discharged by the global thunderstorm activity and air-earth current in the fair weather, respectively. This large-scale electric circuit is termed a global electric circuit. Recently, it is pointed out that the variation of ionospheric potential is associated with global climate change, so that some of scientists started revisiting this traditional topic. In order to promote their resurvey, we show that a ground-based measurement of atmospheric electric field highly affected by atmospheric clouds, aerosols, and so on is still a useful tool to measure the variation of ionospheric potential through the simultaneous observations of ground-based atmospheric electric field, aerosols, and clouds on the R/V Hakuho Maru over the Pacific Ocean. In the period we obtained Carnegie curve, the observed AEF did not correlate to atmospheric aerosol concentration. The most plausible interpretation is that the observed variation of AEF reflected the variation of ionosphere potential.
収録刊行物
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- Journal of Atmospheric Electricity
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Journal of Atmospheric Electricity 34 (1), 21-26, 2014
日本大気電気学会
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詳細情報 詳細情報について
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- CRID
- 1390001204462870272
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- NII論文ID
- 130004848850
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- ISSN
- 09192050
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可