Abstract:Considering the complex nonlinearity and stochastic features of hydrological processes (e.g., precipitation, evapotranspiration, and temperature) and the individual characteristics of a basin, achieving an accurate prediction of discharge is a demanding task (Dinh et al., 2021;Gauch et al., 2021;Hassan & Hassan, 2021). In general, the approaches for streamflow prediction can be categorized into process-driven models
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