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  1. 原著論文

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

https://repo.qst.go.jp/records/47543
https://repo.qst.go.jp/records/47543
e9789a26-f43c-4322-8576-88cb9f584b73
Item type 学術雑誌論文 / Journal Article(1)
公開日 2016-09-06
タイトル
タイトル Diurnal variation of atmospheric electric field at the summit of Mount Fuji, Japan, distinctly different from the Carnegie curve in the summertime
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
アクセス権
アクセス権 metadata only access
アクセス権URI http://purl.org/coar/access_right/c_14cb
著者 Kamogawa, Masashi

× Kamogawa, Masashi

WEKO 476445

Kamogawa, Masashi

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Suzuki, Yuko

× Suzuki, Yuko

WEKO 476446

Suzuki, Yuko

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Sakai, Rikuma

× Sakai, Rikuma

WEKO 476447

Sakai, Rikuma

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Fujiwara, Hironobu

× Fujiwara, Hironobu

WEKO 476448

Fujiwara, Hironobu

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Torii, Tatsuo

× Torii, Tatsuo

WEKO 476449

Torii, Tatsuo

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Kakinami, Yoshihiro

× Kakinami, Yoshihiro

WEKO 476450

Kakinami, Yoshihiro

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Watanabe, Yasuyuki

× Watanabe, Yasuyuki

WEKO 476451

Watanabe, Yasuyuki

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Sato, Ryoe

× Sato, Ryoe

WEKO 476452

Sato, Ryoe

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Hashimoto, Satoshi

× Hashimoto, Satoshi

WEKO 476453

Hashimoto, Satoshi

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Okochi, Hiroshi

× Okochi, Hiroshi

WEKO 476454

Okochi, Hiroshi

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Miura, Kazuhiko

× Miura, Kazuhiko

WEKO 476455

Miura, Kazuhiko

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Yasuda, Hiroshi

× Yasuda, Hiroshi

WEKO 476456

Yasuda, Hiroshi

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Orihara, Yoshiaki

× Orihara, Yoshiaki

WEKO 476457

Orihara, Yoshiaki

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Suzuki, Tomoyuki

× Suzuki, Tomoyuki

WEKO 476458

Suzuki, Tomoyuki

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保田 浩志

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WEKO 476459

en 保田 浩志

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抄録
内容記述タイプ Abstract
内容記述 In fair weather, a clear diurnal variation of atmospheric electric field (AEF), which is distinctly different from the global diurnal variation, i.e., Carnegie curve, was observed during the summer time (July and August) of the year 2010 and 2011 at the summit of Mount Fuji, Japan (3776 m in altitude). The variation of the AEF at the summit showed a local time dependent feature, which means that the AEF increased at sunrise and decreased at sunset. This local diurnal variation is known as a mountain variation. The intensity of AEF in the daytime reached 1.5–3 times larger than that in the nighttime. From the multipoint observations of cloud images and AEF, the mountain variation was found to be attributable to the AEF generated by the positively charged top of a horizontally extensive sea of clouds below the summit. Since the sea of clouds grows with the temperature rise, the AEF variation follows local time.
書誌情報 Geophysical Research Letters

巻 42, 号 8, p. 3019-3023, 発行日 2016-09
出版者
出版者 American Geophysical Union
ISSN
収録物識別子タイプ ISSN
収録物識別子 0094-8276
DOI
識別子タイプ DOI
関連識別子 10.1002/2015GL063677
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