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    1960—2019年哈密市平均风速变化趋势及多尺度特征分析

    Analysis of changing trend and multi-scale characteristics of average wind speed in Hami city from 1960 to 2019

    • 摘要: 精准识别风速时间序列的局部信息,揭示风速变化的内在规律,可为水土保持工作提供重要数据支持及方法论基础。利用哈密市1960—2019年逐日平均风速资料,通过线性趋势分析、突变性检验以及多尺度分解与重构技术,深入探讨哈密市风速的变化趋势与多尺度变化特征。结果表明:1)哈密市近60 a平均风速呈现减小趋势,减小速率为0.0301 m/(s·a),与我国乃至全球地表风速的变化趋势一致,但在2000年以后有小幅度增大现象,且风速的长期变化具有一定的突变性,其年平均风速于1981和1986年发生突变;2)风速序列存在年际尺度和年代际尺度2个典型的固有时间尺度,其中年代际振荡在风速变化中占据主导地位,以30 a为主要变化周期;3)VMD方法在能够有效识别出哈密多年平均风速的非线性变化趋势上效果显著,分解重构的风速序列能够精准表现出哈密风速的长期趋势和短期波形特征,为风速的研究提供了新方法。采用时间序列数据对哈密市平均风速变化进行分析,可提高对该区域风速变化的整体性认识,为未来风速的预测奠定基础,对改善哈密市的生态环境具有重要的意义。

       

      Abstract:
      Background Accurately identifying local information in wind speed time series is crucial for revealing the intrinsic patterns of wind speed variations. Hami city, a typical region for wind speed research, offers valuable insights into local wind speed trends. Previous studies have primarily focused on large-scale wind speed changes at national or regional levels, lacking precise guidance on small-scale variations. Additionally, these studies often relied on wavelet analysis method, resulting in high costs and low efficiency. Building on prior research, this paper introduces new methods to explore small-scale wind speed variations, providing essential data support and a methodological foundation for soil and water conservation efforts.
      Methods The daily average wind speed data from 1960 to 2019 in Hami city were selected, and the final data was obtained through outlier processing and interpolation. The overall trend of the average wind speed in Hami over the years was analyzed using the linear trend method, and the Mann-Kendall method was used to test for abrupt changes in the average wind speed sequence. Empirical mode decomposition was used to identify the inherent change characteristics of the wind speed sequence and reconstruct it.
      Results 1) The average wind speed in Hami city has shown a decreasing trend in the past 60 years, with a decrease rate of 0.0301 m/(s·a), which is consistent with the trend of surface wind speed changes in China and even globally. However, there has been a slight increase since 2000, and the long-term changes in wind speed have a certain degree of abrupt change. The annual average wind speed experienced abrupt changes in 1981 and 1986. 2) There are two typical inherent time scales for wind speed series: interannual scale and decadal scale. Among them, decadal oscillation dominates the wind speed variation, with 30 years as the main variation period. 3) The VMD method is effective in identifying the nonlinear trend of the average wind speed in Hami over the years. The decomposed and reconstructed wind speed sequence can accurately represent the long-term trend and short-term waveform characteristics of Hami wind speed, providing a new method for wind speed research.
      Conclusions By analyzing the changes in average wind speed in Hami city, this study validates the effectiveness of the VMD method in capturing nonlinear trends and multi-scale oscillations in wind speed data. It provides a new approach for wind speed research, enhances our comprehensive understanding of regional wind speed variations, and holds significant importance for improving the ecological environment of Hami city.

       

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