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山地地形对下击暴流风场特性影响的研究

Study on downburst wind field characteristics under mountainous

中文摘要英文摘要

下击暴流为雷暴天气中强下沉气流猛烈冲击地面后形成的并沿地面传播的极具突发性和破坏性的近地面短时强风。从工程结构抗风设计的角度来说,研究下击暴流风场特性,并最终确定合理的下击暴流风剖面是研究的核心目的之一。地形状况是影响下击暴流风场特性的主要因素之一。本文在典型山体地形下击暴流下的近地风场的研究中,利用CFD数值模拟方法计算得到了山体不同位置的速度云图和压力云图,得到了二维山坡典型山体地形的风场分布。

ownburst is a strong downdraft thunderstorm in the ground formed after the violent impact and spread along the ground very sudden and destructive winds near the ground short. From an engineering point of view for the structure of wind-resistant design, researching downburst wind field characteristics and ultimately determining a reasonable downburst wind profile is one of the core objectives of the study. Terrain conditions are the major factors of downburst wind field characteristics .Based on the typical mountain terrain on the wind storm flow condition, this paper established typical 2D slope mountain terrain model, using the method of computational fluid dynamics to calculate the velocity contours and pressure cloud in different locations of the mountain. Finally we get the two-dimensional slope typical mountain terrain wind field distribution.)

吴元泽、孙义、侍海滔、吉柏锋

大气科学(气象学)工程设计、工程测绘

计算流体动力学下击暴流二维山坡风场特性

CFDNumerical Simulationdownburstdimensional hillsidecharacteristics of wind field

吴元泽,孙义,侍海滔,吉柏锋.山地地形对下击暴流风场特性影响的研究[EB/OL].(2014-05-23)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201405-423.点此复制

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