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  1. 防災科研関係論文

Intensive Radiosonde Observations of Environmental Conditions on the Development of a Mesoscale Convective System in the Baiu Frontal Zone

https://nied-repo.bosai.go.jp/records/6688
https://nied-repo.bosai.go.jp/records/6688
77120234-5d30-4c50-938d-b3d865705e75
Item type researchmap(1)
公開日 2024-07-08
タイトル
言語 en
タイトル Intensive Radiosonde Observations of Environmental Conditions on the Development of a Mesoscale Convective System in the Baiu Frontal Zone
著者 A. Manda

× A. Manda

en A. Manda

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Y. Tachibana

× Y. Tachibana

en Y. Tachibana

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H. Nakamura

× H. Nakamura

en H. Nakamura

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T. Takikawa

× T. Takikawa

en T. Takikawa

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A. Nishina

× A. Nishina

en A. Nishina

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Q. Moteki

× Q. Moteki

en Q. Moteki

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N. Zhao

× N. Zhao

en N. Zhao

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S. Iizuka

× S. Iizuka

en S. Iizuka

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抄録
内容記述タイプ Other
内容記述 Abstract

Mesoscale convective systems (MCSs) that occur in the Baiu frontal zone (BFZ) can cause devastating flash floods during early summer in Japan; however, the environmental conditions necessary for their development require further investigation. High‐frequency atmospheric soundings, conducted using multiple marine vessels in the East China Sea on 19 June 2022, captured the detailed environmental conditions pertaining to the development of an MCS within the BFZ. The MCS, which developed rapidly without any remarkable preceding synoptic or mesoscale disturbance in the mid‐ or upper troposphere, caused intense precipitation exceeding 80 mm/hr. The MCS persisted for approximately 6 hr, and it intensified when the influx of nearly saturated air near the sea surface toward a weak surface front overlapped with the influx of free‐tropospheric moist air. The influx of nearly saturated air near the sea surface ensured conditional instability within the lower troposphere. The influx of moist air in the free troposphere contributed to the near‐saturation conditions above the boundary layer, a feature inherent to the BFZ, and played an important role in minimizing the reduction in the buoyancy of air parcels. The results of this study indicate that a better forecast of the horizontal distribution of free tropospheric moist air is beneficial for limiting the potential area of genesis of MCS in the BFZ, and a more comprehensive understanding of the vertical variations in moisture transport contributes to an improved forecast skill for MCS in the BFZ.
言語 en
書誌情報 en : Earth and Space Science

巻 11, 号 7, 発行日 2024-07
出版者
言語 en
出版者 American Geophysical Union (AGU)
ISSN
収録物識別子タイプ EISSN
収録物識別子 2333-5084
DOI
関連識別子 10.1029/2023ea003486
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