Abstract Prolonged drought conditions significantly exacerbate the depletion of water resources. This increases the importance of accurate prediction and preparedness to deal with the negative impacts of drought. This work proposed a deep learning LSTM-based model for predicting drought indices—the Standard Precipitation Index (SPI) and Standardized Precipitation-Evapotranspiration Index (SPEI). To achieve this, two watersheds in Iran were studied, and statistical data from 1972 to 2020 were employed. Several linear and nonlinear methodologies were used to evaluate the proposed model and control models’ results. The mean absolute error (MAE), root mean squared error (RMSE), and R-squared (RS) findings demonstrated that the suggested model outperformed the control models in terms of accuracy ( MAE = 0.057 , RMSE = 0.079 , and RS = 0.0053 ). Similarly, the findings of the difference percentage of Lyapunov exponent (LE) and approximate entropy (ApEn) suggested that the proposed LSTM model was superior compared with the time-series models. Furthermore, a nonlinear dynamic analysis of the ARIMA and LSTM model results demonstrated that the suggested model conserved the dynamic properties of the base time-series better, resulting in more accurate results.
Fattahi et al. (Mon,) studied this question.
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