日本地球惑星科学連合2022年大会

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[J] 口頭発表

セッション記号 A (大気水圏科学) » A-CC 雪氷学・寒冷環境

[A-CC28] 雪氷学

2022年5月26日(木) 15:30 〜 17:00 301B (幕張メッセ国際会議場)

コンビーナ:紺屋 恵子(海洋研究開発機構)、コンビーナ:石川 守(北海道大学)、砂子 宗次朗(防災科学技術研究所)、コンビーナ:舘山 一孝(国立大学法人 北見工業大学)、座長:舘山 一孝(国立大学法人 北見工業大学)


16:15 〜 16:30

[ACC28-07] 格子ボルツマン法を用いた吹きだまりモデルの開発

*丹治 星河1稲津 將2、大風 翼3 (1.北海道大学大学院理学院、2.北海道大学大学院理学研究院、3.東京工業大学大学院環境・社会理工学院)


キーワード:吹雪、吹きだまり、防雪柵、格子ボルツマン法

We developed a snowdrift model to evaluate the snowdrift height around snow fences, which are often installed along roads in snowy, windy locations. The model consisted of the conventional computational fluid dynamics solver that used the lattice Boltzmann method and a module for calculating the snow particles’ motion and accumulation. The calculation domain was a half channel with a flat free-slip boundary on the top and a non-slip boundary on the bottom, and an inflow with artificially generated turbulence from one side to the outlet side was imposed. In addition to the reference experiment with no fence, experiments were set up with a two-dimensional and a three-dimensional fence normal to the dominant wind direction in the channel center. The estimated wind flow over the two-dimensional fence was characterized by a swirling eddy in the cross section, whereas the wind flow in the three-dimensional fence experiment was horizontally diffluent with a dipole vortex pair on the leeward side of the fence. Almost all the snowdrift formed on the windward side of the two-dimensional and three-dimensional fences, although the snowdrift also formed along the split streaks on the leeward side of the three-dimensional fence. Our results suggested that the fence should be as long as possible to avoid snowdrifts on roads.