Abstract

Accurate monitoring and forecasting of drought are crucial. They play a vital role in the optimal functioning of irrigation systems, risk management, drought readiness, and alleviation. In this work, Artificial Intelligence (AI) models, comprising Multi-layer Perceptron Neural Network (MLPNN) and Co-Active Neuro-Fuzzy Inference System (CANFIS), and regression, model including Multiple Linear Regression (MLR), were investigated for multi-scalar Standardized Precipitation Index (SPI) prediction in the Garhwal region of Uttarakhand State, India. The SPI was computed on six different scales, i.e., 1-, 3-, 6-, 9-, 12-, and 24-month, by deploying monthly rainfall information of available years. The significant lags as inputs for the MLPNN, CANFIS, and MLR models were obtained by utilizing Partial Autocorrelation Function (PACF) with a significant level equal to 5% for SPI-1, SPI-3, SPI-6, SPI-9, SPI-12, and SPI-24. The predicted multi-scalar SPI values utilizing the MLPNN, CANFIS, and MLR models were compared with calculated SPI of multi-time scales through different performance evaluation indicators and visual interpretation. The appraisals of results indicated that CANFIS performance was more reliable for drought prediction at Dehradun (3-, 6-, 9-, and 12-month scales), Chamoli and Tehri Garhwal (1-, 3-, 6-, 9-, and 12-month scales), Haridwar and Pauri Garhwal (1-, 3-, 6-, and 9-month scales), Rudraprayag (1-, 3-, and 6-month scales), and Uttarkashi (3-month scale) stations. The MLPNN model was best at Dehradun (1- and 24- month scales), Tehri Garhwal and Chamoli (24-month scale), Haridwar (12- and 24-month scales), Pauri Garhwal (12-month scale), Rudraprayag (9-, 12-, and 24-month), and Uttarkashi (1- and 6-month scales) stations, while the MLR model was found to be optimal at Pauri Garhwal (24-month scale) and Uttarkashi (9-, 12-, and 24-month scales) stations. Furthermore, the modeling approach can foster a straightforward and trustworthy expert intelligent mechanism for projecting multi-scalar SPI and decision making for remedial arrangements to tackle meteorological drought at the stations under study.

Highlights

  • Several drought classifications are mentioned in the literature; they are usually categorized into three main classes: (1) meteorological drought—a scenario where the shortage of precipitation is over 25% from the normal or average volume over an area for some time; (2) hydrological drought—a scenario where the resources of surface water and groundwater begin to exhaust from a marked level; and (3) agricultural drought—a scenario where the soil moisture and rainfall are insufficient in the growing season to boost vigorous crop growth until maturity

  • These models were trained with 70% of the data and tested by deploying 30% data of Standardized Precipitation Index (SPI)-1, 3, 6, 9, 12, and 24 at seven study sites

  • Apart from this, a comparison among Artificial Intelligence (AI) performance (i.e., Co-Active Neuro-Fuzzy Inference System (CANFIS) and Multi-layer Perceptron Neural Network (MLPNN)) and regression (i.e., Multiple Linear Regression (MLR)) models is shown in Table 7, which reveals that the CANFIS gained the highest-ranking followed by the MLPNN at all study sites except the Uttarkashi

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Summary

Introduction

The theoretical definition of drought is expressed generally as the shortage of precipitation causing harm to crops and harvest. The operational description aids people to determine the commencement, rigorousness, and conclusion period of the drought based on 30-year records by comparing the present situation with the historical average (recommended by the World Meteorological Organization). Several drought classifications are mentioned in the literature; they are usually categorized into three main classes: (1) meteorological drought—a scenario where the shortage of precipitation is over 25% from the normal or average volume over an area for some time; (2) hydrological drought—a scenario where the resources of surface water and groundwater begin to exhaust from a marked level; and (3) agricultural drought—a scenario where the soil moisture and rainfall are insufficient in the growing season to boost vigorous crop growth until maturity

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