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  1. 防災科研関係論文

Intensification and maintenance of a double warm-core structure in Typhoon Lan (2017) simulated by a cloud-resolving model

https://nied-repo.bosai.go.jp/records/4967
https://nied-repo.bosai.go.jp/records/4967
b8dd8f0c-3f92-4076-84ad-6a2a46f34867
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Intensification and maintenance of a double warm-core structure in Typhoon Lan (2017) simulated by a cloud-resolving model
言語
言語 eng
著者 Satoki Tsujino

× Satoki Tsujino

en Satoki Tsujino

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Kazuhisa Tsuboki

× Kazuhisa Tsuboki

en Kazuhisa Tsuboki

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Hiroyuki Yamada

× Hiroyuki Yamada

en Hiroyuki Yamada

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Tadayasu Ohigashi

× Tadayasu Ohigashi

en Tadayasu Ohigashi

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Kosuke Ito

× Kosuke Ito

en Kosuke Ito

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Norio Nagahama

× Norio Nagahama

en Norio Nagahama

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抄録
内容記述タイプ Other
内容記述 Knowledge of the development and maintenance processes of double warm cores in tropical cyclones is important for full understanding of the dynamics of storm intensity changes. During its mature stage, Typhoon Lan (2017) had a clear double warm-core structure, which was observed by dropsondes. In this study, to investigate the intensification and maintenance of the double warm-core structure, a numerical simulation of the storm is performed with a cloud-resolving model and verified by dropsonde and satellite observations. A potential temperature budget and backward trajectories are diagnosed to examine intensification and maintenance processes in the simulated eye. The budget analysis indicates that, during the most rapidly intensifying stage, a double warm core is enhanced by axisymmetric subsidence warming in the eye. In the mature stage, upper-core warming is mostly canceled by ventilation due to vertical wind shear, but the lower core continues to warm by asymmetric advection, possibly associated with dynamical instability in the eyewall. The results raise a topic of interest: It is difficult to fully explain the axisymmetric subsidence warming process during the most rapidly intensifying stage by the dynamical response in an axisymmetric balanced vortex. The back-trajectory analysis indicates that the air mass associated with the subsidence is partly induced by inward acceleration in subgradient regions (unbalanced processes) in the eyewall.
言語 en
書誌情報 en : Journal of the Atmospheric Sciences

巻 78, 号 2, p. 595-617, 発行日 2021-02
出版者
言語 en
出版者 American Meteorological Society
ISSN
収録物識別子タイプ EISSN
収録物識別子 1520-0469
DOI
関連識別子 10.1175/jas-d-20-0049.1
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