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Climate variability in different spatial scales is a study area which has reached interest in application, especially during de last years. River discharges can be considered as a robust integrator of the properties of the basin; under these premises the goal of this work is to analyse flows from the Paraná and Uruguay rivers in several gauge stations 5 and study the behavior of positive and negative anomalies and their extremes. The variable to be analysed was defined as the number ofdoi:10.5194/hessd-7-2949-2010 fatcat:krgvaykmdraohlvzpm5pazbspm