Abstract

Hydrological drought forecasting plays a substantial role in water resources management. Hydrological drought highly affects the water allocation and hydropower generation. In this research, short term hydrological drought forecasted based on the hybridized of novel nature-inspired optimization algorithms and Artificial Neural Networks (ANN). For this purpose, the Standardized Hydrological Drought Index (SHDI) and the Standardized Precipitation Index (SPI) were calculated in one, three, and six aggregated months. Then, three states where proposed for SHDI forecasting, and 36 input-output combinations were extracted based on the cross-correlation analysis. In the next step, newly proposed optimization algorithms, including Grasshopper Optimization Algorithm (GOA), Salp Swarm algorithm (SSA), Biogeography-based optimization (BBO), and Particle Swarm Optimization (PSO) hybridized with the ANN were utilized for SHDI forecasting and the results compared to the conventional ANN. Results indicated that the hybridized model outperformed compared to the conventional ANN. PSO performed better than the other optimization algorithms. The best models forecasted SHDI1 with R2 = 0.68 and RMSE = 0.58, SHDI3 with R <sup xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sup> = 0.81 and RMSE = 0.45 and SHDI6 with R <sup xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">2</sup> = 0.82 and RMSE = 0.40.

Highlights

  • Drought is a natural phenomenon that occurs in all climates

  • Salp Swarm algorithm (SSA) performed as the best algorithm in M10 and M11, Biogeography-based optimization (BBO) produced the best results in M3, M7 and M9, Particle Swarm Optimization (PSO) in M2, M5, M6, M8 and M12 and Grasshopper Optimization Algorithm (GOA) in M1 and M4

  • Results indicated that the hybridized models are far superior to the conventional Artificial Neural Networks (ANN), and these models are capable of forecasting the hydrological drought in different time scales

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Summary

Introduction

Drought is a natural phenomenon that occurs in all climates. It is a creeping event with an extensive spatial coverage that the determination of the onset and end of drought is difficult [1]. As the drought occurs in every part of the world eventually, the water resources systems affect by that, and it leads to water shortage in an area during a short to long period. Drought classifies into four types, including meteorological, hydrological, agricultural and socio-economic. It can be said that drought is a progressive phenomenon that starts with a precipitation deficit as a meteorological drought. Prolonged meteorological drought may lead to hydrological drought resulted in decreasing the dam reservoir volume, river flow, and water level in lakes. A sustained hydrological drought leads to agricultural drought

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