基于现场实测的下击暴流时空演化特性研究

RESEARCH ON SPATIOTEMPORAL EVOLUTION CHARACTERISTICS OF DOWNBURSTS UPON FILED MEASUREMENT

  • 摘要: 下击暴流是一种尺度小、持续时间短且破坏性大的极端强风,其风场具有三维特性和显著的非平稳特性,关键风场参数亦随时间演化。为了研究非平稳下击暴流风场特性的时空演化规律,基于北京325 m气象塔现场实测数据,识别并得到典型下击暴流风速记录,研究时变平均风和脉动风的演化特性,包括风速沿高度的相关性、时变平均风速剖面与湍流强度剖面的演化、脉动风速的演化功率谱密度,并对湍流积分尺度和功率谱等关键风场参数进行了分析。研究结果表明:下击暴流沿不同高度上时变平均风速互相关系数达到0.6~0.9,表现出较强的相关性,但其残余脉动风速几乎无相关性;时变平均风速剖面在风速峰值发生时刻表现出下击暴流特有的“鼻形”剖面,而在雷暴发生前后均表现出与大尺度良态风剖面类似的规律;湍流强度在近地面附近大于高度较大处,最大可达0.3;下击暴流实测功率谱与Von Karman谱吻合较好;湍流积分尺度约为9.5 m~29.4 m,远小于大尺度良态风对应的积分尺度;下击暴流残余脉动风速在时域和频域内均表现出明显的非平稳特性,其能量在时域中主要分布在风速的急速突变时期内,在频域内则主要集中在0 Hz~0.1 Hz。

     

    Abstract: Downbursts are extreme winds that are small in scale, short in duration, and severe in destruction. The wind fields have three-dimensional characteristics and significant non-stationary properties, with key wind field parameters evolving over time. In order to study the spatiotemporal evolution characteristics of downburst wind fields, a typical thunderstorm outflow record was identified and obtained by the grounds of the field measurement data collected by the Beijing 325 m meteorological tower, and the evolutionary characteristics of the time-varying mean and fluctuating winds were studied, including the correlation of wind speed along height, the evolution of the time-varying mean wind speed profile and turbulence intensity profile, and the evolutionary power spectral density of the residual fluctuating wind speed. Additionally, key wind field parameters such as turbulence integral scale and power spectrum were also analyzed. The research findings indicate that: the cross-correlation coefficients of the time-varying average wind speed at different heights span from approximately 0.6 to 0.9, denoting a robust correlation, whereas the residual fluctuation has almost no correlation at different heights. The time-varying mean wind speed profile exhibits a distinctive "nose-shaped" profile at the instant of peak wind speed, showing patterns similar to those of large-scale synoptic winds before and after the downburst. The turbulence intensity is markedly higher near the ground compared to aloft, peaking at 0.3. The measured power spectrum of downburst is in a good agreement with the Von Karman spectrum. The turbulence integral scales are determined to be between 9.5 m and 29.4 m, considerably smaller than those for large-scale synoptic winds. The residual fluctuating wind speeds present pronounced non-stationary characteristics in both the time and frequency domain, with energy predominantly distributed during periods of rapid wind speed transitions in the time domain, and mainly concentrated around 0 Hz to 0.1 Hz in the frequency domain.

     

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