Research on the acceleration effect of horizontal wind in mountainous terrain

The utilization of mountain wind resources are important issues in the development of wind energy. However, when wind flows over mountainous terrain, its velocity and direction undergo certain changes, resulting in more complex mountain wind fields and induced structural wind effects. To study the d...

Full description

Bibliographic Details
Main Authors: Lin He, Zheng Zhong’an, Li Xiaojun, Yu Wenshu, Xia Xiang, Ji Wei, Ye Jichao, Wu Jianyong
Format: Article
Language:English
Published: EDP Sciences 2023-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/78/e3sconf_celct2023_01021.pdf
_version_ 1797345624451973120
author Lin He
Zheng Zhong’an
Li Xiaojun
Yu Wenshu
Xia Xiang
Ji Wei
Ye Jichao
Wu Jianyong
author_facet Lin He
Zheng Zhong’an
Li Xiaojun
Yu Wenshu
Xia Xiang
Ji Wei
Ye Jichao
Wu Jianyong
author_sort Lin He
collection DOAJ
description The utilization of mountain wind resources are important issues in the development of wind energy. However, when wind flows over mountainous terrain, its velocity and direction undergo certain changes, resulting in more complex mountain wind fields and induced structural wind effects. To study the distribution characteristics of horizontal wind in mountainous areas, in this study, wind tunnel experiments were conducted on regular mountain models with different slopes to investigate the wind field characteristics at various locations in the mountain range. The research shows that near the mountain surface, the wind speed and velocity ratio follow the order of mountain top > mountain waist > mountain foot, with a wind acceleration effect at the mountain top (wind speed ratio greater than 1) and a wind deceleration effect at the mountain foot and waist (wind speed ratio less than 1). As the height increases, the wind speed ratios gradually approach 1. Moreover, with an increase in slope ratio, the wind speed decreases at the mountain foot and increases at the mountain top. And with the increase of the slope leads to an increasing difference in wind speed ratio between the mountain top and the foot.
first_indexed 2024-03-08T11:20:24Z
format Article
id doaj.art-657ef5a9bc5740b8bac97d9e10b87a2b
institution Directory Open Access Journal
issn 2267-1242
language English
last_indexed 2024-03-08T11:20:24Z
publishDate 2023-01-01
publisher EDP Sciences
record_format Article
series E3S Web of Conferences
spelling doaj.art-657ef5a9bc5740b8bac97d9e10b87a2b2024-01-26T10:02:11ZengEDP SciencesE3S Web of Conferences2267-12422023-01-014410102110.1051/e3sconf/202344101021e3sconf_celct2023_01021Research on the acceleration effect of horizontal wind in mountainous terrainLin He0Zheng Zhong’an1Li Xiaojun2Yu Wenshu3Xia Xiang4Ji Wei5Ye Jichao6Wu Jianyong7Lishui Zhengyang Electric Power Design Institute Co., LtdLishui Zhengyang Electric Power Design Institute Co., LtdLishui Zhengyang Electric Power Design Institute Co., LtdLishui Zhengyang Electric Power Design Institute Co., LtdState Grid Zhejiang Electric Power Co., LtdState Grid Lishui Power Supply CompanyState Grid Lishui Power Supply CompanyState Grid Lishui Power Supply CompanyThe utilization of mountain wind resources are important issues in the development of wind energy. However, when wind flows over mountainous terrain, its velocity and direction undergo certain changes, resulting in more complex mountain wind fields and induced structural wind effects. To study the distribution characteristics of horizontal wind in mountainous areas, in this study, wind tunnel experiments were conducted on regular mountain models with different slopes to investigate the wind field characteristics at various locations in the mountain range. The research shows that near the mountain surface, the wind speed and velocity ratio follow the order of mountain top > mountain waist > mountain foot, with a wind acceleration effect at the mountain top (wind speed ratio greater than 1) and a wind deceleration effect at the mountain foot and waist (wind speed ratio less than 1). As the height increases, the wind speed ratios gradually approach 1. Moreover, with an increase in slope ratio, the wind speed decreases at the mountain foot and increases at the mountain top. And with the increase of the slope leads to an increasing difference in wind speed ratio between the mountain top and the foot.https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/78/e3sconf_celct2023_01021.pdf
spellingShingle Lin He
Zheng Zhong’an
Li Xiaojun
Yu Wenshu
Xia Xiang
Ji Wei
Ye Jichao
Wu Jianyong
Research on the acceleration effect of horizontal wind in mountainous terrain
E3S Web of Conferences
title Research on the acceleration effect of horizontal wind in mountainous terrain
title_full Research on the acceleration effect of horizontal wind in mountainous terrain
title_fullStr Research on the acceleration effect of horizontal wind in mountainous terrain
title_full_unstemmed Research on the acceleration effect of horizontal wind in mountainous terrain
title_short Research on the acceleration effect of horizontal wind in mountainous terrain
title_sort research on the acceleration effect of horizontal wind in mountainous terrain
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/78/e3sconf_celct2023_01021.pdf
work_keys_str_mv AT linhe researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT zhengzhongan researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT lixiaojun researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT yuwenshu researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT xiaxiang researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT jiwei researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT yejichao researchontheaccelerationeffectofhorizontalwindinmountainousterrain
AT wujianyong researchontheaccelerationeffectofhorizontalwindinmountainousterrain