日本地球惑星科学連合2025年大会

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[E] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS02] 台風研究の新展開~過去・現在・未来

2025年5月25日(日) 13:45 〜 15:15 102 (幕張メッセ国際会議場)

コンビーナ:辻野 智紀(気象研究所)、金田 幸恵(名古屋大学宇宙地球環境研究所)、伊藤 耕介(京都大学防災研究所)、宮本 佳明(慶應義塾大学 環境情報学部)、座長:金田 幸恵(名古屋大学宇宙地球環境研究所)

14:30 〜 14:45

[AAS02-10] Formation of long-lasting inactive and active multiple tropical cyclone events in the western North Pacific

*Lilan Chen1、Jianyun Gao1、Tim Li2 (1.Fujian Institute of Meteorological Sciences、2.University of Hawaii at Manoa)

キーワード:Multiple tropical cyclone events, intraseasonal oscillation, PMM-like SST anomaly, Indian Ocean warming

Long-lasting inactive and active multiple tropical cyclone (MTC) events in the western North Pacific (WNP) during July-August 1982-2020 were investigated. It is found that the significant difference between the inactive and active events lies on large-scale circulation conditions and tropical SST anomalies in the Pacific and Indian Ocean. A negative phase of the Pacific Meridional Mode (PMM), an Indian ocean warming and a local suppressed convective phase are associated with the long-lasting inactive MTC events, and vice versa. A further diagnosis of the environmental parameters showed that dynamic parameters such as mid-level vertical motion and the upper-level divergence and thermodynamic parameters such as vertically integrated water vapor content and low-level specific humidity play important roles in regulating the inactive and active MTC events. A separation of interannual and intraseasonal components indicates that the extreme MTC events are influenced by both the timescale motions. While the former is primarily through the SSTA-induced low-level anticyclonic and descent anomalies, the latter is via the fluctuation of the boreal summer atmospheric intraseasonal oscillation.