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Research on the relationship between rainfall and reference crop evapotranspiration with multi-time scales

机译:多时间尺度下降雨与参考作物蒸散量关系的研究

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Limited by Fourier analysis and the selection of different wavelet base functions, the wavelet analysis method shows some deficiencies. For that reason, the empirical mode decomposition method is applied to analyze fluctuating periods and local features of annual rainfall and reference crop evapotranspiration (ET0) from 1959 to 2002. With respect to the correlation between variables, the traditional time series analysis methods often assume that data sequences are stationary which result in "spurious regression." Therefore, the cointegration theory is introduced to describe the long-term equilibrium relationship of rainfall and ET0. At last, to understand the uncertainty between these two variables, the set pair analysis (SPA) method is used to present the identity, discrepancy, and contrary of rainfall and ET0 with multi-time scales. The results reveal that rainfall and ET0 have a complex relationship which may be related to El Nino, air-sea intersection, solar activity. Moreover, the fluctuation periods of rainfall and ET0 also have similar short and middle period level, and slightly different long period level. The changes of rainfall and ET0 present mainly the contrary and the discrepancy. This relationship will remain a long-term equilibrium.
机译:受傅立叶分析和不同小波基函数选择的限制,小波分析方法显示出一些缺陷。因此,采用经验模式分解方法来分析1959年至2002年年降水量和参考作物蒸散量(ET0)的波动周期和局部特征。关于变量之间的相关性,传统的时间序列分析方法通常假定数据序列是固定的,导致“虚假回归”。因此,引入协整理论来描述降雨与ET0的长期平衡关系。最后,为了了解这两个变量之间的不确定性,使用集对分析(SPA)方法来表示多时间尺度下降雨和ET0的标识,差异和相反。结果表明,降雨与ET0的关系复杂,可能与厄尔尼诺现象,海气交叉,太阳活动有关。此外,降雨和ET0的波动周期也具有相似的中短期水平,而长期水平略有不同。降雨和ET0的变化主要呈现相反和差异性。这种关系将保持长期平衡。

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