日本地球惑星科学連合2024年大会

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[J] 口頭発表

セッション記号 H (地球人間圏科学) » H-DS 防災地球科学

[H-DS11] 津波とその予測

2024年5月31日(金) 10:45 〜 12:00 国際会議室 (IC) (幕張メッセ国際会議場)

コンビーナ:馬場 俊孝(徳島大学大学院産業理工学研究部)、室谷 智子(国立科学博物館)、座長:馬場 俊孝(徳島大学大学院産業理工学研究部)、Kirill Sementsov(Hokkaido University, Faculty of Science, Institute of Seismology and Volcanology)

10:45 〜 11:00

[HDS11-01] Predicting Tsunami Run-Up Characteristics through Comprehensive Computational Fluid Dynamics Analysis

*Peiwei Xie1、Yan Du1 (1.South China Sea Institute of Oceanology, Chinese Academy of Science)

キーワード:tsunami , numerical simulation , run-up height, run-up velocity , swash period

Accurate estimation of tsunami run-up is crucial for effective forecasting and early warning systems, yet developing a sufficiently reliable model remains a challenge. This study employs a self-manipulated Computational Fluid Dynamics (CFD) model to systematically simulate and analyze tsunami run-up characteristics. The simulations encompass a wide range of surf-similarity (0.9 to 11.9) and wave nonlinearity (0.1 to 8.9), leading to the formulation of novel run-up estimation methods. Our results reveal that, under fixed surf-similarity, tsunamis on mild slopes exhibit easier breaking, resulting in lower run-up heights compared to steep slopes. Waves with strong non-linearity experience more intense deformation and dynamics during their run-up than those with weaker non-linearity. We propose a semi-empirical method for conservative estimations of tsunami run-up height and velocity, relying on onsite wave measurements along the slope, thereby eliminating the need for arbitrary input from the beach's toe or offshore areas. Notably, this method demonstrates feasibility for waves with non-linearity up to 2.0, indicating its applicability across a broad spectrum of conditions. Additionally, we introduce an empirical formula for swash period estimation. Despite inherent limitations, the proposed method and formula present potential contributions to the toolkit for tsunami forecasts and early warnings, offering insights and alternative avenues for further exploration in this complex field.