Abstract

Drought forecasting plays a crucial role in drought mitigation actions. Thus, this research deals with linear stochastic models (autoregressive integrated moving average (ARIMA)) as a suitable tool to forecast drought. Several ARIMA models are developed for drought forecasting using the Standardized Precipitation Evapotranspiration Index (SPEI) in a hyper-arid climate. The results reveal that all developed ARIMA models demonstrate the potential ability to forecast drought over different time scales. In these models, the p, d, q, P, D and Q values are quite similar for the same SPEI time scale. This is in correspondence with autoregressive (AR) and moving average (MA) parameter estimate values, which are also similar. Therefore, the ARIMA model (1, 1, 0) (2, 0, 1) could be considered as a general model for the Al Qassim region. Meanwhile, the ARIMA model (1, 0, 3) (0, 0, 0) at 3-SPEI and the ARIMA model (1, 1, 1) (2, 0, 1) at 24-SPEI could be generalized for the Hail region. The ARIMA models at the 24-SPEI time scale is the best forecasting models with high R2 (more than 0.9) and lower values of RMSE and MAE, while they are the least forecasting at the 3-SPEI time scale. Accordingly, this study recommends that ARIMA models can be very useful tools for drought forecasting that can help water resource managers and planners to take precautions considering the severity of drought in advance.

Highlights

  • Water demand has significantly increased in many parts of the world, especially in hyper-arid regions that are facing a shortage of available water resources

  • The Standardized Precipitation Evapotranspiration Index (SPEI) is presented as a powerful multi-scalar drought index to investigate drought event variations in Al-Qassim and Hail regions

  • The first part of the objective is the assessment of climatic parameters and drought frequency based on SPEI

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Summary

Introduction

Water demand has significantly increased in many parts of the world, especially in hyper-arid regions that are facing a shortage of available water resources. World-climatic change is leading to more droughts on the Earth’s surface [1]. Floods and droughts projected for the 21st century show large significant changes from those in the 20th century [3]. The impact of intense long drought on natural ecosystems essentially concerns regional agriculture, water resources and the environment [4]. The lack of a precise assessment of drought in certain situations may lead to incorrect decisions and actions by managers and policy makers [5]. Scientists categorized the drought phenomenon into four major groups: meteorological, agricultural, hydrologic and socio-economic [6,7]

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