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This paper describes the numerical study of nonstratified airflow over a real complex terrain. Attention is focused on the mechanism of a local strong wind induced by a topographic effect. In order to clarify the mechanism of the occurrence of strong winds accompanied by the effects of terrain, the use of a numerical simulation is very effective, in which conditions can be set without the influence of ground roughness and temperature distribution. As a result, airflow converged to a small basin of mountain terrain in the upper stream, and local strong wind was generated leeward along the slope of the mountain terrain. Furthermore, the influence of the reproduction accuracy of geographical features, that is, horizontal grid resolution, was examined. Consequently, to reproduce the above-mentioned local strong wind, it was shown that horizontal grid resolution from 50 m to about 100 m was necessary.
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篇名 Numerical Prediction of Strong Wind Induced by Topographic Effect
来源期刊 流体动力学(英文) 学科 地球科学
关键词 CFD LES Complex TERRAIN Local STRONG WIND Topographic Effect GRID RESOLUTION
年,卷(期) ltdlxyw_2019,(3) 所属期刊栏目
研究方向 页码范围 224-240
页数 17页 分类号 P4
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研究主题发展历程
节点文献
CFD
LES
Complex
TERRAIN
Local
STRONG
WIND
Topographic
Effect
GRID
RESOLUTION
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研究来源
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研究去脉
引文网络交叉学科
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期刊影响力
流体动力学(英文)
季刊
2165-3852
武汉市江夏区汤逊湖北路38号光谷总部空间
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302
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0
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