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Interannual variability in the Uruguay river basin

机译:乌拉圭河流域的年际变化

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Both (El Nino-southern oscillation ENSO)-scale and near-decadal variations in precipitation and river flow have been noted in southeastern South America. Here we focus on the Uruguay river basin and its subcatchments. Both river flow and precipitation are analysed with singular spectrum analysis in an examination of how the signals of the subcatchments are related to the overall basin signal. The approximate 6 year signal and the 3.5 year ENSO signal are the two statistically significant peaks for the river flow. Both signals are present in all the available river flows, but only in the precipitation of the upper two-thirds of the basin. Precipitation in the lower part of the basin shows positive trends. The ENSO signal is strongly modulated at the secular time scale; we construct a simple sinusoidal model for this modulation.
机译:在南美东南部,降水和河流流量的(厄尔尼诺南极涛动ENSO)规模和近十年的变化都被注意到。在这里,我们重点介绍乌拉圭河流域及其子汇水面积。通过检查子汇水面积的信号与流域整体信号之间的关系,使用奇异频谱分析法分析了河流流量和降水。大约6年的信号和3.5年的ENSO信号是河流流量的两个具有统计意义的峰值。这两种信号都存在于所有可用的河流中,但仅出现在流域上部三分之二的降水中。流域下部的降水呈积极趋势。 ENSO信号在世俗时间尺度上受到强烈调制;我们为此调制构建了一个简单的正弦模型。

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