日本地球惑星科学連合2025年大会

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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-AS09] 応用気象学

2025年5月27日(火) 10:45 〜 12:15 展示場特設会場 (4) (幕張メッセ国際展示場 7・8ホール)

コンビーナ:稲津 將(北海道大学大学院理学研究院)、竹見 哲也(京都大学防災研究所)、日下 博幸(筑波大学)、座長:丹治 星河(京都大学)

10:45 〜 11:00

[AAS09-01] Estimating the effect of snowdrift formation on turbulent airflow and subsequent snowdrift around three-types of fences

*丹治 星河1 (1.京都大学)

キーワード:吹雪、格子ボルツマン法、吹きだまり、防雪柵、Large-eddy simulation

We investigated the effect of formed snowdrifts in advance on the turbulent flow and subsequent snowdrift distribution around three types of snow fences in a numerical simulation. The simulation for an 8 h drifting snow event was conducted with updating the bottom boundaries following the snowdrift structure every 2 h. The calculation domains were flat ground surfaces installed three types of solid fences—two-dimensional fence, three-dimensional fence, and two-dimensional fence with a bottom gap. Snowdrift height on the windward side of the two-dimensional fence was higher in the updating experiment than in no-updating one because wind profiles and snow trajectories were modified depending on the previous snowdrift shapes. Around the three-dimensional and bottom-gap fences, differences of snowdrift height between with and without updating bottom boundaries were generated on the leeward areas. Snowdrifts on the leeward side of these fences were formed on far areas in the no-updating experiment, but the experiment considering the previous snowdrift structures developed snowdrifts closer to the fence. These results suggested that snowdrift development on the leeward side of obstacles could be overestimated if the previous snowdrift structure were neglected in numerical simulations.