Quantifying Drought Impacts Based on the Reliability–Resiliency–Vulnerability Framework over East Africa

Author:

Babaousmail Hassen1,Ayugi Brian Odhiambo2ORCID,Hammad Zulfiqar2,Alupot Donnata34,Posset Kokou Romaric4,Mumo Richard56ORCID,Rajasekar Adharsh7ORCID

Affiliation:

1. School of Atmospheric Science and Remote Sensing, Wuxi University, Wuxi 214105, China

2. Faculty of Civil Engineering, Seoul National University of Science and Technology, 232 Gongneung-ro, Nowon-gu, Seoul 01811, Republic of Korea

3. Uganda National Meteorological Authority, Port Bell Road Luzira, Kampala P.O. Box 7025, Uganda

4. Pan African University Institute for Water and Energy Sciences (including Climate Change), c/o Université Abou Bekr Belkaid Tlemcen, B.P. 119, Campus Chetouane, Tlemcen 13000, Algeria

5. Department of Mathematics and Statistical Sciences, Botswana International University of Science and Technology, Palapye Plot 10071, Botswana

6. Department of Statistics and Actuarial Science, Dedan Kimathi University of Technology, Nyeri P.O. Box 657-10100, Kenya

7. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Centre on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, China

Abstract

Drought poses a significant threat to water resources in East Africa, necessitating a comprehensive assessment of its impacts for effective mitigation strategies. This study utilizes two global gridded SPEI datasets to analyze drought characteristics (i.e., frequency, duration, and severity) in East Africa from 1981 to 2021. To estimate the sustainability of water resources over the region, the study employed the Reliability–Resiliency–Vulnerability framework (RRV) that aggregates the drought characteristics (i.e., frequency, duration, and severity). Drought is deemed to have occurred when the SPEI value falls below −1, so the threshold for water demand (RRV) is also computed at a threshold level of −1. The findings indicate pronounced changes in drought patterns across East Africa, with evidence of varying degrees of recovery and resilience in different regions. Employing the RRV framework over the East Africa region to determine how the region can cope with the effects of drought revealed a median range of RRV of 0.61 to 0.80, indicating a sustainable situation during the study period. This indicates that despite the recorded drought incidences, the water catchments of lakes, rivers, and major water towers are not threatened and, thus, less vulnerable. Although certain regions exhibit declining resilience and vulnerability to drought impacts, there is a need for targeted mitigation measures and policy interventions to safeguard water resources.

Funder

discount vouchers from the journal

Publisher

MDPI AG

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