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Power spectral characteristics of drought indices in the Ebro river basin at different temporal scales

机译:不同时间尺度下埃布罗河流域干旱指数的功率谱特征

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摘要

A deep spectral investigation of the monthly time series of Standardized Precipitation Index (SPI) and Standardized Precipitation Evapotranspiration Index (SPEI) in 45 meteorological stations in the Ebro basin (Spain) from 1950 to 2006 for timescales ranging from 1 to 48 months was performed. In order to summarize the results for the whole basin, the spectral analysis was also carried out on the four principal components of SPI and SPEI. Results confirm that SPI and SPEI presents very similar spectral characteristics. At the shorter time scales, the signal of SPI and SPEI is characterized by purely random temporal fluctuations. The longer time scales tend to feature the signal as a smoothly varying time series or persistent, mostly due to the aggregated nature of the indices calculation. The comparative analysis of the spectral properties of the drought indices for all the 45 sites in the Ebro basin lead to the identification of global or regional effects discriminated by local effects. It was found that some periodical signals are common to almost all the sites, while others where only identified in specific meteorological stations.
机译:对1950年至2006年西班牙埃布罗盆地45个气象站的标准降水指数(SPI)和标准降水蒸发蒸腾指数(SPEI)的每月时间序列进行了深入的频谱调查,其时间范围为1至48个月。为了总结整个盆地的结果,还对SPI和SPEI的四个主要成分进行了光谱分析。结果证实SPI和SPEI具有非常相似的光谱特性。在更短的时间范围内,SPI和SPEI的信号具有纯随机的时间波动特征。较长的时间标度趋向于将信号表现为平滑变化的时间序列或持续存在,这主要是由于指标计算的汇总性质。对埃布罗河流域所有45个地点的干旱指数光谱特性的比较分析导致确定了以局部影响为特征的全球或区域影响。结果发现,几乎所有站点都具有某些周期性的信号,而其他信号仅在特定的气象站才能识别。

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