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May-August global multivariate ENSO index (MEI) correlated with October-January streamflow at Algarrobal for (a) positive MEI years, (b) all MEI years, and (c) negative MEI years. 

May-August global multivariate ENSO index (MEI) correlated with October-January streamflow at Algarrobal for (a) positive MEI years, (b) all MEI years, and (c) negative MEI years. 

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In many semi-arid regions, multisectoral demands often stress available water supplies. Such is the case in the Elqui River valley of northern Chile, which draws on a limited-capacity reservoir to allocate 25 000 water rights. Delayed infrastructure investment forces water managers to address demand-based allocation strategies, particularly in dry...

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... The results are consistent with other streamflow prediction studies in the same basin, although they have different methodologies in terms of predictive performance. Likewise, they are consistent with the fact that predictive performance in the ERB tends to decrease as the prediction lead time increases [65]. In addition, the results are positive compared to those obtained historically on an official basis by the General Water Directorate of Chile in this basin, as studies indicate that no forecast performed in northern Chile has entered the "good forecast" category [43]. ...
... Regarding the most important variables for prediction, Figure 5 shows the mean importance of the variables by prediction model. prediction lead time increases [65]. In addition, the results are positive compared to those obtained historically on an official basis by the General Water Directorate of Chile in this basin, as studies indicate that no forecast performed in northern Chile has entered the "good forecast" category [43]. ...
... Indeed, El Niño has presented less predictive ability in the last decade due to the influence of other ocean climate factors, with the 500 hPa geopotential height in the Amundsen-Bellingshausen sector standing out [42,67]. Figure 6a,b presents the partial dependence plots (PDP), also known as partial dependence profiles, for both models, to show how the expected prediction value behaves as a function of some variable of interest, using the most important variable in each model [56,62,63]. The graphs highlight two important aspects for interpretation: first, it is observed that the individual ceteris paribus (CP) profiles, similar to the individual conditional expectation (ICE) plots, are parallel, which is indicative of an additive model without interaction between predictors, and facilitating extrapolation in the predictor space by making the PDP adequately represent the profile of each instance [56,65,68]. Second, the graphs show that for values between −1 and 1 SD from the predictor mean, the estimated streamflow at Río Elqui en Algarrobal presents a low linear increase, although it is clearly staggered throughout the prediction domain. ...
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... It typically combines hydrological models with ensemble Quantitative Precipitation Forecasts (QPF), resulting in probabilistic estimates of future streamflow (Cloke and Pappenberger, 2009), and the QPF are the source of information on the future water input. This method has been widely used in different works (Buizza et al., 2005;De Paiva et al., 2020;Delorit et al., 2017;Demirel et al., 2015;Hersbach, 2000;Van Dijk et al., 2013;Van Hateren et al., 2019). ...
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