日本地球惑星科学連合2025年大会

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[E] ポスター発表

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-AS03] Extreme Events and Mesoscale Weather: Observations and Modeling

2025年5月27日(火) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:竹見 哲也(京都大学防災研究所)、Nayak Sridhara(Japan Meteorological Corporation)、下瀬 健一(国立研究開発法人防災科学技術研究所)、本田 匠(東京大学情報基盤センター)

17:15 〜 19:15

[AAS03-P16] High Resolution Numerical Simulation of Tornado Outbreak associated with Typhoon ShanShan 2024 using Supercomputer Fugaku

*塚越 栞奈1,2、真島 祐介3、本田 巧3、湯上 伸弘3,2吉田 龍二2佐藤 正樹2筆保 弘徳2坪木 和久1,2 (1.名古屋大学宇宙地球環境研究所、2.横浜国立大学台風科学技術研究センター、3.富士通株式会社)


キーワード:竜巻、スーパーセル、アウターレインバンド、スーパーコンピュータ

Tornadoes associated with tropical cyclones cause significant damage in various countries, making their understanding and numerical forecast are a crucial challenge. This study aims to forecast tornadoes by a numerical model and conducts high-resolution numerical simulations at a horizontal resolution of 80 m in across the entire tropical cyclone using large-scale parallel computing on the Fugaku supercomputer.
The case study focuses on the tornado outbreak that occurred in the Kyushu region of Japan in association with Typhoon ShanShan 2024. This event was one of the most significant tornado outbreaks in Japan, with over ten instances of severe wind damages, including five tornadoes classified as the Japan Enhanced Fujita Scale (JEF) 2, with estimated wind speeds exceeding 65 m/s.
Numerical simulations were conducted using the Cloud Resolving Storm Simulator (CReSS, Tsuboki 2023), including a horizontal 500 m grid simulation and a one-way nested horizontal 80 m grid simulation, both of simulation covering the entire typhoon including outer rainband.
For this experiment, 8,192 nodes of the Fugaku supercomputer (approximately 5% of the total nodes) were utilized. To accelerate computation in large-scale parallel processing, simulation processing mapping for Fugaku's server network structure was optimized and overlapped execution of computation and file output were implemented.
As a result, mini-supercells continuously formed in the typhoon’s outer rainbands, and strong vertical vorticity (>0.5 /s) on the tornado scale was detected in the hook echo regions of multiple mini-supercells. Additionally, the 4-hour forecast time simulation and united files output was completed in approximately 1.5 hours elapsed time. These results indicate that predicting tornado forecast in associated with tropical cyclones are feasible with a sufficient lead time of more than two hour.