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  1. 防災科研関係論文

Mesoscale and microscale structures of snow clouds over the Sea of Japan. Part III: Two types of circulations in snow bands associated with a wind-speed-increase zone preceding cold-air outbreaks

https://nied-repo.bosai.go.jp/records/5544
https://nied-repo.bosai.go.jp/records/5544
70ba9d1f-2b1c-45dc-a849-6d514bfe2996
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Mesoscale and microscale structures of snow clouds over the Sea of Japan. Part III: Two types of circulations in snow bands associated with a wind-speed-increase zone preceding cold-air outbreaks
言語
言語 eng
著者 Yoshinori Yamada

× Yoshinori Yamada

en Yoshinori Yamada

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Masataka Murakami

× Masataka Murakami

en Masataka Murakami

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Hakaru Mizuno

× Hakaru Mizuno

en Hakaru Mizuno

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Takayo Matsuo

× Takayo Matsuo

en Takayo Matsuo

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Yasushi Fujiyoshi

× Yasushi Fujiyoshi

en Yasushi Fujiyoshi

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Koyuru Iwanami

× Koyuru Iwanami

en Koyuru Iwanami

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抄録
内容記述タイプ Other
内容記述 Airflow structures in two snow bands, one in 1990 and the other in 1992, over the Sea of Japan have been studied by dual-Doppler radar and supplementary observations. These snow bands appeared in a wind-speed-increase zone, which moved into the experiment area several hours before the outbreak of the winter monsoon. In the 1990 case, dropsonde observations showed that the stratification of low-level air behind the trailing edge of the band was convectively unstable, and that a cold pool was situated beneath the band. A cold air presence was confirmed, also for the 1992 case, from surface temperature analyses. The mass transport budget analyses revealed the relative importance of a band-normal wind component to a mean airflow structure in the both snow bands. Their airflow structures in the band-transverse vertical cross-sections were, however, completely different from each other. The circulation in the 1990 case was characterized by the ascending inflow from the trailing edge and the descending outflow from the leading edge. For the 1992 case, the circulation was the reverse of the 1990 case, the ascending inflow being from the leading edge and the downdraft occurring in the very narrow region around the trailing edge. The different circulations in the two snow bands were explained by vertical wind shear in the band-transverse components of the horizontal winds.
言語 en
書誌情報 en : Journal of the Meteorological Society of Japan

巻 74, 号 5, p. 593-615, 発行日 1996
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/jmsj1965.74.5_593
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