Time-space characterization of droughts in the São Francisco river catchment using the Standard Precipitation Index and continuous wavelet transform

Pub Date : 2019-01-01 DOI:10.1590/2318-0331.241920180092
M. Santos, V. Costa, W. Fernandes, R. P. D. Paes
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引用次数: 13

Abstract

ABSTRACT This paper focuses on time-space characterization of drought conditions in the São Francisco River catchment, on the basis of wavelet analysis of Standardized Precipitation Index (SPI) time series. In order to improve SPI estimation, the procedures for regional analysis with L-moments were employed for defining statistically homogeneous regions. The continuous wavelet transform was then utilized for extracting time-frequency information from the resulting SPI time series in a multiresolution framework and for investigating possible teleconnections of these signals with those obtained from samples of the large-scale climate indexes ENSO and PDO. The use of regional frequency analysis with L-moments resulted in improvements in the estimation of SPI time series. It was observed that by aggregating regional information more reliable estimates of low frequency rainfall amounts were obtained. The wavelet analysis of climate indexes suggests that the more extreme dry periods in the study area are observed when the cold phase of both ENSO and the PDO coincides. While not constituting a strict cause effect relationship, it was clear that the more extreme droughts are consistently observed in this situation. However, further investigation is necessary for identifying particularities in rainfall patterns that are not associated to large-scale climate anomalies.
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基于标准降水指数和连续小波变换的 o Francisco河流域干旱的时空特征
基于标准化降水指数(SPI)时间序列的小波分析,研究了奥弗朗西斯科河流域干旱的时空特征。为了改进SPI估计,采用l矩区域分析程序来定义统计上均匀的区域。然后利用连续小波变换从得到的SPI时间序列中提取多分辨率框架下的时频信息,并研究这些信号与大尺度气候指数ENSO和PDO样本中获得的信号可能存在的远相关。利用l矩的区域频率分析改善了SPI时间序列的估计。据观察,通过汇总区域信息,可以获得更可靠的低频降雨量估计。气候指数的小波分析表明,当ENSO和PDO的冷相重合时,研究区极端干旱期出现的频率更高。虽然不构成严格的因果关系,但很明显,在这种情况下一贯观察到更极端的干旱。然而,需要进一步调查以确定与大尺度气候异常无关的降雨模式的特殊性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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