Análise espectral do sinal geofísico - exemplos de aplicação da transformada de ondeleta

Júlia Amorim, L. Prado, Elder Yokoyama
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Abstract

The study of natural signals demands robust techniquest to allow comprehension of active physical mechanisms. However, many of these signals show non-stationary characteristics, whose average rate varies over time, preventing the applications of classic spectral methods, such as the periodogram. The wavelet transform is a robust tool for non-stationary time series analysis and its use has spread in this field due to its ease of application through subroutines in several softwares. In this work, we present wavelet transform applied to two series of natural signals: number of sunspots and precipitation in Brasilia, Central Brazil. The goal was to identify cycles in both series and relate them to phenomena described in the literature, through the wavelet transform. Results showed a spectral peak at 11 years in Sunspot Series, related to Schwabe's cycle. For the Precipitation Series, a primary spectral peak of 21 years was identified, probably related to the temperature variance in the Pacific Ocean, and secondary cyclicity in 10-16 months. These results confirm the wavelet transform as a robust and satisfactory tool in the spectral study of non-stationary series.
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地球物理信号的光谱分析。小波变换的应用实例
自然信号的研究需要强大的技术来理解主动的物理机制。然而,许多这些信号显示出非平稳特征,其平均速率随时间变化,阻碍了经典频谱方法的应用,如周期图。小波变换是一种鲁棒的非平稳时间序列分析工具,由于它易于在一些软件中通过子程序应用,因此在该领域的应用已经广泛。在这项工作中,我们提出了小波变换应用于两个系列的自然信号:太阳黑子的数量和降水在巴西中部巴西利亚。目的是通过小波变换识别两个序列中的循环,并将它们与文献中描述的现象联系起来。结果表明,太阳黑子序列的光谱峰值出现在11年,与Schwabe周期有关。降水序列的主要谱峰周期为21 a,可能与太平洋温度变化有关,次要周期为10 ~ 16个月。这些结果证实了小波变换在非平稳序列的谱研究中是一种鲁棒和令人满意的工具。
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