Japan Geoscience Union Meeting 2025

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS09] Applied Meteorology

Tue. May 27, 2025 10:45 AM - 12:15 PM Exhibition Hall Special Setting (4) (Exhibition Hall 7&8, Makuhari Messe)

convener:Masaru Inatsu(Faculty of Science, Hokkaido University), Tetsuya Takemi(Disaster Prevention Research Institute, Kyoto University), Hiroyuki Kusaka(University of Tsukuba), Chairperson:Seika Tanji(Kyoto University)

10:45 AM - 11:00 AM

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

*Seika Tanji1 (1.Kyoto University)

Keywords:Drifting snow, Lattice Boltzmann method, Snowdrift, Snow fence, 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.