日本地球惑星科学連合2023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-AS05] 大規模な水蒸気場と組織化した雲システム

2023年5月26日(金) 13:45 〜 15:15 201A (幕張メッセ国際会議場)

コンビーナ:高須賀 大輔(東京大学大気海洋研究所)、横井 覚(海洋研究開発機構)、三浦 裕亮(国立大学法人 東京大学大学院 理学系研究科 地球惑星科学専攻)、濱田 篤(富山大学)、座長:高須賀 大輔(東京大学大気海洋研究所)、濱田 篤(富山大学)

14:15 〜 14:30

[AAS05-03] Preliminary validation of the applicability of the multigrid method to multi-scale representation of fluids

*上野 和雅1三浦 裕亮1 (1.東京大学)

キーワード:マルチグリッド法、マルチスケールモデル、浅水波方程式

Multiscale models perform calculations using multiple lengths and time scales to represent hierarchical structures in the atmosphere and ocean. They can be broadly classified into two methods: systematic asymptotics and superparameterization (Grooms & Julien, 2018). On the other hand, the multigrid method is a method that efficiently reduces errors by proceeding with calculations while changing the grid size and is a beneficial computational method, especially for elliptic boundary value problems (Trottenberg, 2007). In this study, the shallow water wave equation was solved using the multigrid method as a first step to verify the possibility of multiscale representation using the multigrid method. The correspondence between each layer of the multigrid method and the multiscale representation was verified. The results showed that for the semi-implicit discretization method used in this study, the values at each layer are linear interpolations of the values at the finest layer when the multigrid method is applied as is. The results also showed that the appearance of the solution differs depending on the time interval, suggesting the need to introduce multiple length scales in the time direction.