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首页> 外文期刊>Stochastic environmental research and risk assessment >Time-frequency characterization of sub-divisional scale seasonal rainfall in India using the Hilbert-Huang transform
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Time-frequency characterization of sub-divisional scale seasonal rainfall in India using the Hilbert-Huang transform

机译:基于希尔伯特-黄变换的印度分区尺度季节性降雨的时频特征

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Time-frequency characterization is useful in understanding the nonlinear and non-stationary signals of the hydro-climatic time series. The traditional Fourier transform, and wavelet transform approaches have certain limitations in analyzing non-linear and non-stationary hydro-climatic series. This paper presents an effective approach based on the Hilbert-Huang transform to investigate time-frequency characteristics, and the changing patterns of sub-divisional rainfall series in India, and explored the possible association of monsoon seasonal rainfall with different global climate oscillations. The proposed approach integrates the complete ensemble empirical mode decomposition with adaptive noise algorithm and normalized Hilbert transform method for analyzing the spectral characteristics of two principal seasonal rainfall series over four meteorological subdivisions namely Assam-Meghalaya, Kerala, Orissa and Telangana subdivisions in India. The Hilbert spectral analysis revealed the dynamic nature of dominant time scales for two principal seasonal rainfall time series. From the trend analysis of instantaneous amplitudes of multiscale components called intrinsic mode functions (IMFs), it is found that both intra and inter decadal modes are responsible for the changes in seasonal rainfall series of different subdivisions and significant changes are noticed in the amplitudes of inter decadal modes of two seasonal rainfalls in the four subdivisions since 1970s. Further, the study investigated the links between monsoon rainfall with the global climate oscillations such as Quasi Bienniel Oscillation (QBO), El Nino Southern Oscillation (ENSO), Sunspot Number (SN), Atlantic Multidecadal Oscillation (AMO) etc. The study noticed that the multiscale components of rainfall series IMF1, IMF2, IMF3, IMF4 and IMF5 have similar periodic structure of QBO, ENSO, SN, tidal forcing and AMO respectively. As per the seasonal rainfall patterns is concerned, the results of the study indicated that for Assam-Meghalaya subdivision, there is a likelihood of extreme rare events at similar to 0.2 cycles per year, and both monsoon and pre-monsoon rainfall series have decreasing trends; for Kerala subdivision, extreme events can be expected during monsoon season with shorter periodicity (similar to 2.5 years), and monsoon rainfall has statistically significant decreasing trend and post-monsoon rainfall has a statistically significant increasing trend; and for Orissa subdivision, there are chances of extremes rainfall events in monsoon season and a relatively stable rainfall pattern during post-monsoon period, but both monsoon and post-monsoon rainfall series showed an overall decreasing trend; for Telangana subdivision, there is a likelihood of extreme events during monsoon season with a periodicity of similar to 4 years, but both monsoon and post-monsoon rainfall series showed increasing trends. The results of correlation analysis of IMF components of monsoon rainfall and five climate indices indicated that the association is expressed well only for low frequency modes with similar evolution of trend components.
机译:时频表征有助于理解水文气候时间序列的非线性和非平稳信号。传统的傅里叶变换和小波变换方法在分析非线性和非平稳水文气候序列时有一定的局限性。本文提出了一种基于希尔伯特-黄(Hilbert-Huang)变换的有效方法,以研究印度的时频特征以及分区降雨序列的变化模式,并探讨了季风季节降雨与全球气候振荡的可能联系。拟议的方法将完整的综合经验模式分解与自适应噪声算法和归一化的希尔伯特变换方法相结合,以分析印度的Assam-Meghalaya,Kerala,Orissa和Telangana四个分区的两个主要季节性降雨序列的频谱特征。希尔伯特频谱分析揭示了两个主要季节性降雨时间序列的主导时间尺度的动态性质。从被称为固有模式函数(IMF)的多尺度分量瞬时振幅的趋势分析中,可以发现年代际和年代际模式都对不同分区的季节性降雨序列变化起着重要作用,而且自1970年代以来四个分区的两个季节性降雨的年代际模式。此外,该研究还研究了季风降雨与全球气候振荡之间的联系,例如准Bienniel振荡(QBO),厄尔尼诺南部涛动(ENSO),黑子数(SN),大西洋多年代际振荡(AMO)等。研究注意到,降雨序列IMF1,IMF2,IMF3,IMF4和IMF5的多尺度分量分别具有类似的QBO,ENSO,SN,潮汐强迫和AMO周期结构。根据季节性降雨模式,研究结果表明,对于阿萨姆邦-梅加拉亚邦细分,每年极有可能发生罕见的事件,类似于每年0.2个周期,季风和季风前的降雨序列都有下降的趋势;对于喀拉拉邦细分,可以预料到季风季节将出现极端事件,周期较短(约2.5年),季风降雨具有统计上显着的下降趋势,季风后降雨具有统计学上的显着增长趋势;对于奥里萨邦(Orissa)分区,在季风季节有可能出现极端降雨事件,并且在季风后时期有相对稳定的降雨模式,但季风和季风后的降雨序列均显示总体下降趋势;对于Telangana分区,在季风季节有可能发生极端事件,周期类似于4年,但季风和季风后的降雨序列均呈上升趋势。季风降雨的IMF分量与5个气候指数的相关分析结果表明,该关联仅在具有相似趋势分量演化的低频模式中表达良好。

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