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  1. 防災科研関係論文

Structure of two adjacent shear lines accompanied by wind gusts in the Japan Sea coastal region during a cold-air outbreak on 12 December 2010

https://nied-repo.bosai.go.jp/records/5554
https://nied-repo.bosai.go.jp/records/5554
caa94ece-81fc-456a-8fd6-c5841a129c49
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Structure of two adjacent shear lines accompanied by wind gusts in the Japan Sea coastal region during a cold-air outbreak on 12 December 2010
言語
言語 eng
著者 Wataru Mashiko

× Wataru Mashiko

en Wataru Mashiko

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Hanako Y. Inoue

× Hanako Y. Inoue

en Hanako Y. Inoue

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Syugo Hayashi

× Syugo Hayashi

en Syugo Hayashi

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Kenichi Kusunoki

× Kenichi Kusunoki

en Kenichi Kusunoki

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Syunsuke Hoshino

× Syunsuke Hoshino

en Syunsuke Hoshino

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Kenichiro Arai

× Kenichiro Arai

en Kenichiro Arai

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Kenichi Shimose

× Kenichi Shimose

en Kenichi Shimose

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Masako Kusume

× Masako Kusume

en Masako Kusume

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Masahide Nishihashi

× Masahide Nishihashi

en Masahide Nishihashi

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Hiroshi Yamauchi

× Hiroshi Yamauchi

en Hiroshi Yamauchi

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Osamu Suzuki

× Osamu Suzuki

en Osamu Suzuki

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Hiroyuki Morishima

× Hiroyuki Morishima

en Hiroyuki Morishima

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抄録
内容記述タイプ Other
内容記述 c 2012, the Meteorological Society of Japan. Two adjacent shear lines accompanied by wind gusts exceeding 20 m s-1 passed over the Shonai region on the Japan Sea coast during a moderate cold-air outbreak on 12 December 2010. The structure of the shear lines were examined using simulation results and observational data including high-frequency upper-air soundings. Simulation results revealed that cold-airmass outflow from the Eurasian Continent had a split-flow pattern due to the blocking effect of the Changbai Mountains. One is from the south side of the mountains (SCF), and the other is from the north side (NCF). NCF also has two streams: a shallow southward-meandering flow on the south and a slightly deeper straight flow on the north. A shallow shear line was formed between SCF and the shallow southward-meandering flow of NCF. The deeper straight flow of NCF sharply formed another shear line on the north at around 1-km height with SCF. This result implies that the shear lines accompanied by wind gusts on the Japan Sea coast during a coldair outbreak have various structures and that the horizontal wind shear a little above the surface could cause surface wind gusts.
言語 en
書誌情報 en : Scientific Online Letters on the Atmosphere

巻 8, 号 1, p. 90-93, 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.2012-023
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