Abstract

Water resources have always been a major concern, particularly in arid and semiarid parts of the world. Low precipitation and its uneven distribution in Algeria, along with fast population and agriculture activity increase and, particularly, recent droughts, have made water availability one of the country’s most pressing issues. The objectives of the studies reported in this article are to investigate and forecast the meteorological and hydrological drought in Wadi Ouahrane basin (270 km2) using linear stochastic models known as Autoregressive Integrated Moving Average (ARIMA) and multiplicative Seasonal Autoregressive Integrated Moving Average (SARIMA). In particular, data from 6 precipitation stations and 1 hydrometric station for the period 1972–2018 were used to evaluate the Standardized Precipitation Index (SPI) and the Standardized Runoff Index (SRI) for 12 months. Then, the multiplicative ARIMA model was applied to forecasting drought based on SPI and SRI. As a result, the ARIMA model (1,0,1)(0,0,1)12 for SPI and (1,0,1)(1,0,1)12 for SRI were shown to be the best models for drought forecast. In fact, both models exhibited high quality for SPI and SRI of 0.97 and 0.51 for 1-month and 12-month lead time, respectively, based on validation R2. In general, prediction skill decreases with increase in lead time. The models can be used with reasonable accuracy to forecast droughts with up to 12 months of lead time.

Highlights

  • Assessment of Drought Based on Standardized Precipitation Index (SPI) and Standardized Runoff Index (SRI)

  • The popularity of the Autoregressive Integrated Moving Average (ARIMA) model in many areas is due to its flexibility and the systematic searching at each stage for an appropriate model [18]

  • Comparison of multiplicative Seasonal Autoregressive Integrated Moving Average (SARIMA) models used in meteorological and hydrological droughts shows that increasing the forecast lead time increases the error rate

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Summary

Introduction

Drought is a recurring temporary natural phenomenon that generally results from a decrease in precipitation relative to its long-term average and can occur in any climate [1]. An exact drought definition is not simple, as different drought types exist, which can be defined based on the several hydrometeorological variables related to drought, including precipitation, soil moisture, river flow, water level, and groundwater level. To distinguish meteorological drought the precipitation variable is used, to distinguish agricultural drought the soil moisture variable is used, and other hydrological cycle variables are used to diagnose hydrological drought [2,3]. Known as the source of other types of droughts. Hydrological and agricultural droughts arise from meteorological droughts [4]

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