日本地球惑星科学連合2021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] Extreme Events: Observations and Modeling

2021年6月6日(日) 09:00 〜 10:30 Ch.07 (Zoom会場07)

コンビーナ:Sridhara Nayak(Disaster Prevention Research Institute, Kyoto University)、竹見 哲也(京都大学防災研究所)、Satoshi Iizuka(National Research Institute for Earth Science and Disaster Resilience)、座長:Satoshi Iizuka(National Research Institute for Earth Science and Disaster Resilience)、Sridhara Nayak(Disaster Prevention Research Institute, Kyoto University)、竹見 哲也(京都大学防災研究所)

09:45 〜 10:00

[AAS02-04] Influence of Warm SST in the Oyashio Region on Rainfall Distribution of Typhoon Hagibis (2019)

*飯塚 聡1、川村 隆一2、中村 尚3、美山 透4 (1.防災科学技術研究所、2.九州大学大学院理学府地球惑星科学専攻、3.東京大学 先端科学技術研究センター、4.海洋研究開発機構)

キーワード:台風、降水、海面水温、親潮

Typhoon Hagibis (2019) caused widespread flooding and damage over eastern Japan. The associated rainfall maxima were primarily observed on the windward mountain slopes along with the west of the leading edge of a low-level front. Concomitantly, a significant positive value in sea surface temperature anomalies (SSTAs) was observed in association with an ocean eddy over the Oyashio region, together with anomalous warmth over the entire western North Pacific. The present study examines the role of the SSTAs in the rainfall distribution associated with Hagibis, to deepen our understanding of the influence of the midlatitude ocean on tropical cyclones and associated rainfall. Our sensitivity experiments demonstrate that the observed warm SSTAs had the potential to displace the rainfall caused by Hagibis inland and thereby acted to increase precipitation along the Pacific coast of northeastern Japan. Our results suggest that midlatitude SSTAs on ocean-eddy scales can also influence the synoptic-scale atmospheric front and associated heavy rainfall.