稳态雷暴冲击风风速剖面模型研究

邹鑫1,汪之松1,2,,李正良1,2

振动与冲击 ›› 2016, Vol. 35 ›› Issue (15) : 74-79.

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振动与冲击 ›› 2016, Vol. 35 ›› Issue (15) : 74-79.
论文

稳态雷暴冲击风风速剖面模型研究

  • 邹鑫1,汪之松1,2,,李正良1,2
作者信息 +

Study on wind velocity profile of steady thunderstorm downburst

  • ZOU xin1, WANG zhisong1, 2, LI zhengliang1, 2
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文章历史 +

摘要

雷暴冲击风是非台风地区形成极值风荷载的主要原因。采用静止型冲击射流装置和大涡模拟分别对雷暴冲击风风场进行了物理试验和数值模拟,考察了径向风速和竖向风速的分布特征。将大涡模拟结果和试验结果与现有实测数据和理论模型进行了对比,验证了试验和数值模拟结果的可靠性。针对现有的径向风速模型并不适用于所有径向位置处径向风速的问题,结合物理实验和大涡模拟的结果,提出了沿径向变化的径向风速剖面模型。同时,根据风场竖向风速的特点将其沿径向位置分为三个区域,给出了三个区域竖向风速剖面模型。

Abstract

Thunderstorm downburst is the main reason for the formation of extreme wind loads in the non-typhoon area. In this paper, both static impinging jet instrument and large eddy simulation (LES) have been used to do the experiment and numerical simulation for thunderstorm downburst. The distribution of radial and vertical velocity has been investigated. Given the existing radial velocity profile model doesn’t apply to the radial velocity at all radial locations, combined the experiment and LES results, a new radial velocity profile which suits all radial locations is  proposed. Meanwhile, the wind flied is divided into three part according to the characteristic of vertical velocity, the vertical velocity profile is presented for all the three part.

关键词

雷暴冲击风 / 冲击射流模型 / 大涡模拟 / 风场特性

引用本文

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邹鑫1,汪之松1,2,,李正良1,2. 稳态雷暴冲击风风速剖面模型研究[J]. 振动与冲击, 2016, 35(15): 74-79
ZOU xin1, WANG zhisong1, 2, LI zhengliang1, 2. Study on wind velocity profile of steady thunderstorm downburst[J]. Journal of Vibration and Shock, 2016, 35(15): 74-79

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