基于实测数据的台风边界层风速剖面特征研究

黄希桂; 罗胜昌; 李利孝

doi:10.3724/j.gyjzG23121101

基于实测数据的台风边界层风速剖面特征研究

doi: 10.3724/j.gyjzG23121101

黄希桂¹,
罗胜昌^2,3,
李利孝^2,3, ,

1. 哈尔滨工业大学(深圳)土木与环境工程学院, 广东深圳 518055;
2. 深圳大学土木与交通工程学院, 广东深圳 518060;
3. 深圳大学城市智慧交通与安全运维研究院, 广东深圳 518060

基金项目:

国家自然科学基金(52178491)；广东省自然科学基金(2021A1515011769)；深圳市自然科学基金(JCYJ20210324093809023)。

详细信息

作者简介:
黄希桂,硕士,主要从事高层建筑抗风研究。

通讯作者:
李利孝,博士,主要从事结构风工程研究,lilixiao@szu.edu.cn。

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出版历程
- 收稿日期: 2023-12-11
- 网络出版日期: 2024-04-23

Research on Wind Speed Profile Characteristics of Typhoon Boundary Layer Based on Measured Data

1. School of Civil and Environmental Engineering, Harbin university of Technology, Shenzhen 518055, China;
2. College of Civil and Transportation Engineering, Shenzhen University, Shenzhen 518060, China;
3. Institute of Urban Smart Transportation & Safety Maintenance, Shenzhen University, Shenzhen 518060, China

摘要

摘要: 目前规范中对台风影响区建筑物的抗风设计采用类比非气旋风场的方式来进行,然而大量实测结果表明台风剖面与非气旋风场风剖面存在较大差异,风剖面的影响因素和变化规律目前仍不明确。为清晰地了解台风的剖面特征及其规律,基于多个台风的实测剖面数据,以下垫面类型、台风结构分区和风速大小三类控制指标对数据进行分类,对各个类别的风剖面数据进行对比分析。研究表明:台风剖面中的近地急流层与下垫面类型、台风结构分区和风速均有关,即A、B类场地、较大风速和台风后眼壁区更易出现近地急流层;台风风剖面的梯度风高度与下垫面类型和平均风速存在着一定关系,A、B类场地的梯度风高度由台风中心向外呈增大趋势,C类场地下的梯度风高度从台风中心向外呈先减小后增大趋势。
- 台风 /
- 边界层 /
- 风剖面特征 /
- 低空急流 /
- 现场实测
Abstract: The wind-resistant design of building structures in the typhoon affected area in the codes is carried out by analogy with the non-cyclonic wind field, however, many measured results show that there is a large difference between the typhoon wind profile and the profile of the non-cyclonic wind field, and the influencing factors and changing rules of the typhoon wind profile are still not clear at present. To clearly understand the profile characteristics of typhoons, many measured profile data of several typhoons were used for the analysis. The measured data were categorized by three factors, namely, the underlying surface categories, the typhoon structural partitions,and the wind speed, and the wind profile data of each category were comparatively analyzed, and the study showed that: the low-level jet phenomena in typhoon wind profiles was related to the underlying surface categories, the typhoon structural partitions, and the wind speed, the low-level jets were more likely to occur at exposure category A, B, larger wind speed, and in the back eyewall region in typhoon; there was a certain relationship between the gradient wind height of the typhoon wind profile and the type of underlying surface and average wind speed. The gradient wind height of exposure category A and B showed an increasing trend from the center of the typhoon outward, while the gradient wind height underground of exposure category C showed a decreasing and then increasing trend from the center of the typhoon outward.
- typhoon /
- boundary layer /
- wind profile characteristics /
- low-level jet /
- field measurement

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参考文献(25)

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