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  1. 防災科研関係論文

Case study of misoscale convective echo behavior associated with cumulonimbus development observed by Ka-band Doppler radar in the Kanto region, Japan

https://nied-repo.bosai.go.jp/records/5555
https://nied-repo.bosai.go.jp/records/5555
574e8693-c467-4849-9763-bc0b2440e84b
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Case study of misoscale convective echo behavior associated with cumulonimbus development observed by Ka-band Doppler radar in the Kanto region, Japan
言語
言語 eng
著者 Namiko Sakurai

× Namiko Sakurai

en Namiko Sakurai

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Koyuru Iwanami

× Koyuru Iwanami

en Koyuru Iwanami

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Takeshi Maesaka

× Takeshi Maesaka

en Takeshi Maesaka

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Shin Ichi Suzuki

× Shin Ichi Suzuki

en Shin Ichi Suzuki

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Shingo Shimizu

× Shingo Shimizu

en Shingo Shimizu

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Ryohei Misumi

× Ryohei Misumi

en Ryohei Misumi

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Dong Soon Kim

× Dong Soon Kim

en Dong Soon Kim

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Masayuki Maki

× Masayuki Maki

en Masayuki Maki

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抄録
内容記述タイプ Other
内容記述 Simultaneous observations of cumulonimbi by a Ka-band Doppler radar (KaDR) and an X-band polarimetric Doppler radar (MP-X) were performed during the summer of 2011 in the Kanto region, Japan to study the process of cumulonimbus initiation and development. A cumulonimbus developed up to 12 km above sea level (ASL) in the mountainous western part of the Kanto region on the morning of 18 August 2011, and its initiation and development were observed by the two radars. A misoscale convective echo which was newly detected in an RHI or PPI scan and developed vertically (RHI scan) or spatially (PPI scan) was labeled as a 'new misoscale convective echo' (NMCE). In the developing stage (DS), NMCEs occurred one after another, and the echo top height and maximum reflectivity of each individual echo gradually increased. In the first half of the DS, the NMCEs appeared between 2 and 5 km ASL. In contrast, in the second half of the DS, the NMCEs' appearance height stepped up to between 5 and 12 km ASL. These results suggest that the ascent of NMCE appearance height is one of the key factors in the prediction of deep convection, which later causes localized heavy rainfall.
言語 en
書誌情報 en : Scientific Online Letters on the Atmosphere

巻 8, 号 1, p. 107-110, 発行日 2012
ISSN
収録物識別子タイプ EISSN
収録物識別子 1349-6476
DOI
関連識別子 10.2151/sola.2012-027
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