首页> 外文期刊>大气科学进展(英文版) >Performance of the Wind Farm Parameterization Scheme Coupled with the Weather Research and Forecasting Model under Multiple Resolution Regimes for Simulating an Onshore Wind Farm
【24h】

Performance of the Wind Farm Parameterization Scheme Coupled with the Weather Research and Forecasting Model under Multiple Resolution Regimes for Simulating an Onshore Wind Farm

机译:风电场参数化方案结合多分辨率条件下天气研究与预报模型的性能模拟陆上风电场

获取原文
获取原文并翻译 | 示例
       

摘要

We use the Wind Farm Parameterization (WFP) scheme coupled with the Weather Research and Forecastingmodel under multiple resolution regimes to simulate turbulent wake dynamics generated by a real onshore wind farm and their influence at the local meteorological scale.The model outputs are compared with earlier modeling and observation studies.It is found that higher vertical and horizontal resolutions have great impacts on the simulated wake flow dynamics.The corresponding wind speed deficit and turbulent kinetic energy results match well with previous studies.In addition,the effect of horizontal resolution on near-surface meteorology is significantly higher than that of vertical resolution.The wake flow field extends from the start of the wind farm to downstream within 10 km,where the wind speed deficit may exceed 4%.For a height of 150 m or at a distance of about 25 km downstream,the wind speed deficit is around 2%.This indicates that,at a distance of more than 25 km downstream,the impact of the wind turbines can be ignored.Analysis of near-surface meteorology indicates a night and early morning warming near the surface,and increase in near-surface water vapor mixing ratio with decreasing surface sensible and latent heat fluxes.During daytime,a slight cooling near the surface and decrease in the near-surface water vapor mixing ratio with increasing surface sensible and latent heat fluxes is noticed over the wind farm area.
机译:我们将风电场参数化(WFP)方案与天气研究和预报模型结合使用,在多种分辨率模式下模拟真实陆上风电场产生的湍流尾流动力学及其在当地气象尺度上的影响,并将模型输出与早期建模进行比较研究发现,较高的垂直和水平分辨率对模拟的尾流动力学有很大的影响。相应的风速赤字和湍动能结果与以前的研究相吻合。地面气象学明显高于垂直分辨率。尾流流场从风电场的开始一直延伸到10公里以内的下游,在那里风速赤字可能超过4%。在150 m的高度或距离为下游约25 km,风速赤字约为2%。这表明,在下游25 km以上的距离,风力涡轮机的影响可以忽略不计。近地表气象分析表明,地表有夜间和清晨变暖,并且近地表水汽混合比增加,且表面感热和潜热通量减小。在风电场范围内,随着地表感热和潜热通量的增加,地表附近的空气冷却和近地表水蒸汽混合比降低。

著录项

  • 来源
    《大气科学进展(英文版)》 |2019年第2期|119-132|共14页
  • 作者单位

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    University of Chinese Academy of Sciences, Beijing 100049, China;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号