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Exploring the role of reanalysis data in simulating regional wind generation variability over Northern Ireland

机译:探索重新分析数据在模拟北爱尔兰地区风力发电变化中的作用

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摘要

As wind generation increases, system impact studies rely on predictions of future generation and effective representation of wind variability. A well-established approach to investigate the impact of wind variability is to simulate generation using observations from 10 m meteorological mast-data. However, there are problems with relying purely on historical wind-speed records or generation histories: mast-data is often incomplete, not sited at a relevant wind generation sites, and recorded at the wrong altitude above ground (usually 10 m), each of which may distort the generation profile. A possible complimentary approach is to use reanalysis data, where data assimilation techniques are combined with state-of-the-art weather forecast models to produce complete gridded wind time-series over an area. Previous investigations of reanalysis datasets have placed an emphasis on comparing reanalysis to meteorological site records whereas this paper compares wind generation simulated using reanalysis data directly against historic wind generation records. Importantly, this comparison is conducted using raw reanalysis data (typical resolution ~50 km), without relying on a computationally expensive "dynamical downscaling" for a particular target region. Although the raw reanalysis data cannot, by nature of its construction, represent the site-specific effects of sub-gridscale topography, it is nevertheless shown to be comparable to or better than the mast-based simulation in the region considered and it is therefore argued that raw reanalysis data may offer a number of significant advantages as a data source.
机译:随着风力发电量的增加,系统影响研究依赖于对未来发电量的预测以及对风力变化性的有效表示。一种成熟的研究风变率影响的方法是使用来自10 m气象桅杆数据的观测结果来模拟发电。但是,仅依靠历史风速记录或发电历史存在问题:桅杆数据通常是不完整的,不位于相关的风力发电站,而是在错误的地面海拔高度(通常为10 m)记录,每个这可能会扭曲生成配置文件。一种可能的补充方法是使用重新分析数据,其中数据同化技术与最新的天气预报模型相结合,以在一个区域上生成完整的网格风时间序列。以前对再分析数据集的研究一直侧重于将再分析与气象站点记录进行比较,而本文将使用再分析数据模拟的风力直接与历史风力记录进行了比较。重要的是,该比较是使用原始的重新分析数据(典型分辨率约为50 km)进行的,而不依赖于特定目标区域的计算上昂贵的“动态缩小”。尽管原始的重新分析数据不能根据其构造的性质来表示子网格地形的特定站点影响,但是在所考虑的区域中,它仍可与基于桅杆的模拟进行比较或优于其,因此有人提出了争议。原始的重新分析数据可以作为数据源提供许多重要的优势。

著录项

  • 来源
    《Renewable energy 》 |2013年第9期| 558-561| 共4页
  • 作者单位

    Technologies for Sustainable Built Environments Centre, University of Reading, Reading, Berkshire RC6 6UR, United Kingdom;

    National Centre for Atmospheric Sciences, University of Reading, Reading, United Kingdom, Department of Meteorology, University of Reading, Reading United Kingdom;

    School of Construction Management and Engineering, University of Reading, United Kingdom;

    Technologies for Sustainable Built Environments Centre, University of Reading, Reading, Berkshire RC6 6UR, United Kingdom, Department of Meteorology, University of Reading, Reading United Kingdom;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    reanalysis; wind-simulation; wind generation; variability; intermittency; boundary layer wind-shear;

    机译:重新分析风模拟风力发电变化性;间歇性边界层风切变;

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