Journal of Water and Climate Change (Feb 2023)

Drought characterization and severity analysis using GRACE-TWS and MODIS datasets: a case study from the Awash River Basin (ARB), Ethiopia

  • Yitea Seneshaw Getahun,
  • Ming-Hsu Li,
  • Yi-Ying Chen,
  • Tewoderos Addisu Yate

DOI
https://doi.org/10.2166/wcc.2023.361
Journal volume & issue
Vol. 14, no. 2
pp. 516 – 542

Abstract

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Drought is the utmost highly devastating phenomenon in Ethiopia because of societies that are reliant on rainfall-dependent agriculture; thus, it is crucial to characterize drought at the basin scale using new developments in remote sensing products and recently proposed drought indices. This study aimed to quantify drought in the Awash River Basin (ARB) using drought indices of the Standardized Precipitation Index (SPI), Standardized Precipitation Evapotranspiration Index (SPEI), Evaporative Demand Drought Index (EDDI), Evaporative Stress Index (ESI), and Water Storage Deficit Index (WSDI). The Mann–Kendall test analysis of annual and seasonal terrestrial water storage (TWS) showed a significant increase from 2002 to 2017 that is beneficial for developmental activities in the ARB. GRACE showed a record high extreme drought that persisted for 15 months was noticed from 2005/01 to 2006/03 with a total water storage deficit of −411.8 mm with a peak shortage of −46.24 mm in 2005/03, representing severe terrestrial water shortage in the ARB. This GRACE-TWS-based quantified extreme water shortage in 2005/30 can be used as a threshold for adaptation. Overall, this study provides a reliable outcome that will be vital for the establishment of climate change adaptation pathways in the future for viable water resources management to minimize the disastrous impacts of drought in the AR. HIGHLIGHTS TWS showed a significantly increasing trend in the basin with an annual rate of 3.6 mm/year.; A significant TWS deficit was observed before 2009, and a significant increase afterward.; The SPI, SPEI, ESI, and EDDI indices highly correlated at 3- and 6-month time scales.; GRACE-based, i.e. a total water deficit of −411.8 mm is a useful threshold for climate change adaptation.;

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