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  1. 防災科研関係論文

Behavior and structure of convective clouds developing around a mountainous area observed by stereo photogrammetry and ka-band and x-band radars: Case study of northern Kanto, Japan

https://nied-repo.bosai.go.jp/records/5515
https://nied-repo.bosai.go.jp/records/5515
37192f9c-453f-426f-ad2b-7d58e1bad4ee
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Behavior and structure of convective clouds developing around a mountainous area observed by stereo photogrammetry and ka-band and x-band radars: Case study of northern Kanto, Japan
言語
言語 eng
著者 Natsuki Nishiwaki

× Natsuki Nishiwaki

en Natsuki Nishiwaki

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Ryohei Misumi

× Ryohei Misumi

en Ryohei Misumi

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Shingo Shimizu

× Shingo Shimizu

en Shingo Shimizu

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Takeshi Maesaka

× Takeshi Maesaka

en Takeshi Maesaka

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Koyuru Iwanami

× Koyuru Iwanami

en Koyuru Iwanami

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Namiko Sakurai

× Namiko Sakurai

en Namiko Sakurai

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Masayuki Maki

× Masayuki Maki

en Masayuki Maki

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Shin-Ichi Suzuki

× Shin-Ichi Suzuki

en Shin-Ichi Suzuki

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Atsushi Kato

× Atsushi Kato

en Atsushi Kato

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Akihiko Yamaji

× Akihiko Yamaji

en Akihiko Yamaji

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抄録
内容記述タイプ Other
内容記述 Development of convective clouds on August 24, 2009 in northern Kanto, Japan, was investigated using stereo photogrammetric analysis and Ka-band and X-band radars, in order to clarify the behavior and structure of convective clouds developing around a mountainous area. Convective activity was divided into three stages based on the spatial distribution of X-band radar echoes: stage 1 with no echo (1006-1200 JST), stage 2 with echoes limited to the mountainous area (1200-1400 JST), and stage 3 with echoes developing over the plain (1400-1600 JST). During stages 1 and 2, the convective clouds (echoes) initiated over the mountains, and then moved toward the foot of mountains and dissipated, repeatedly. During stage 3, convective echoes formed over the mountains moved to the plain without dissipating at the foot of the mountains. In stage 2, new convective echoes tended to form to the rear (upshear) side of pre-existing echoes, while in stage 3, some new cellular echoes formed to the front (downshear) side of pre-existing echoes. Specific humidity in the mountains increased in stage 1, while GPS-derived precipitable water at the foot of the mountains increased during stages 2 and 3. The relationship between the behavior of convective clouds and the transport of water vapor by local wind circulation is discussed. c 2013, Meteorological Society of Japan.
言語 en
書誌情報 en : Journal of the Meteorological Society of Japan

巻 91, 号 5, p. 609-626, 発行日 2013
出版者
言語 en
出版者 Meteorological Society of Japan
ISSN
収録物識別子タイプ ISSN
収録物識別子 0026-1165
DOI
関連識別子 10.2151/jmsj.2013-504
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