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  1. 防災科研関係論文

A mechanism of the onset of the Australian summer monsoon

https://nied-repo.bosai.go.jp/records/4464
https://nied-repo.bosai.go.jp/records/4464
d95d8930-4818-47f5-b083-cd7c1ef7cd95
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル A mechanism of the onset of the Australian summer monsoon
言語
言語 eng
著者 Ryuichi Kawamura

× Ryuichi Kawamura

en Ryuichi Kawamura

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Yuichiro Fukuta

× Yuichiro Fukuta

en Yuichiro Fukuta

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Hiroaki Ueda

× Hiroaki Ueda

en Hiroaki Ueda

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Tomonori Matsuura

× Tomonori Matsuura

en Tomonori Matsuura

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Satoshi Iizuka

× Satoshi Iizuka

en Satoshi Iizuka

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抄録
内容記述タイプ Other
内容記述 [1] An onset mechanism of the Australian summer monsoon that incorporates possible air-sea feedback processes is investigated using the National Centers for Environmental Prediction /National Center for Atmospheric Research daily reanalysis data aided by an ocean general circulation model. Rapid intensification of land-ocean thermal contrast during the premonsoon period results in a well-organized continental-scale shallow vertical circulation over the Australian continent. The shallow vertical circulation is dynamically coupled both with a thermally induced low at the lower level below 850 hPa and a thermal high at 600-700 hPa level. Intensified low-level westerly anomalies and increased solar radiation in less cloudy air induced by the subsidence in the periphery of the Australian thermal low results in increasing sea surface temperature (SST) along the northern coast of Australia. The thermal high concurrent with the shallow vertical circulation leads to dry intrusion into the layer at similar to700 hPa over the Arafura Sea and Coral Sea through the horizontal and vertical advective processes. A combination of the SST increase and the dry intrusion creates a more convectively unstable condition. When convective instability is intensified while subsidence suppresses convection, the arrival of large-scale disturbances with ascending motion (such as the Madden-Julian oscillation) at the domain where the instability is enhanced triggers deep cumulus convection, implying the onset of the monsoon. The onset mechanism proposed in this study may apply not only to the Australian monsoon but also to other monsoon systems that have continental masses in the subtropics.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES

巻 107, 号 D14
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ ISSN
収録物識別子 0747-7309
DOI
関連識別子 10.1029/2001JD001070
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