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Resolving Nonstationary Spectral Information in Wind Speed Time Series Using the Hilbert-Huang Transform

机译:使用Hilbert-Huang变换解决风速时间序列中的非平稳光谱信息

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This work is motivated by the observation that large-amplitude wind fluctuations on temporal scales of 1-10 h present challenges for the power management of large offshore wind farms. Wind fluctuations on these scales are analyzed at a meteorologicalmeasurement mast in the Danish North Sea using a 4-yr time series of 10-min wind speed observations. An adaptive spectral analysis method called the Hilbert-Huang transform is chosen for the analysis, because the nonstationarity of time series of wind speed observations means that they are not well described by a global spectral analysis method such as the Fourier transform. The Hilbert-Huang transform is a local method based on a nonparametric and empirical decomposition of the data followed by calculation of instantaneous amplitudes and frequencies using the Hilbert transform. The Hilbert-Huang transformed 4-yr time series is averaged and summarized to show climatological patterns in the relationship between wind variability and time of day. First, by integrating the Hilbert spectrum along the frequency axis, a scalar time series representing the total variability within a given frequency range is calculated. Second, by calculating average spectra conditional to time of day, the time axis of the Hilbert spectrum is "remapped" to show climatological patterns. Third, the daily patterns in wind variability and wind speed are compared for the four seasons of the year. It is found that the most intense wind variability occurs in autumn even though the strongest observed wind speeds occur in winter.
机译:这项工作的动机是观察到,在1到10小时的时间尺度上,大幅度风的波动对大型海上风电场的电力管理提出了挑战。使用4年的10分钟风速观测时间序列,在丹麦北海的一个气象测量桅杆上分析了这些尺度的风波动。选择一种称为Hilbert-Huang变换的自适应频谱分析方法进行分析,因为风速观测的时间序列的非平稳性意味着它们无法通过诸如Fourier变换之类的全局频谱分析方法很好地描述。 Hilbert-Huang变换是基于数据的非参数和经验分解,然后使用Hilbert变换计算瞬时幅度和频率的局部方法。对希尔伯特-黄(Hilbert-Huang)变换的4年时间序列进行平均和汇总,以显示风向变化与一天中时间之间关系的气候模式。首先,通过沿频率轴对希尔伯特频谱进行积分,可以计算出表示给定频率范围内总可变性的标量时间序列。其次,通过计算以一天中某个时间为条件的平均光谱,希尔伯特光谱的时间轴被“重新映射”以显示气候模式。第三,比较一年中四个季节的日风变化和风速。发现最大的风变率发生在秋季,即使观察到的最大风速发生在冬季。

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