Extreme hydroclimatic variability and impact of local and global climate system anomalies on extreme flow in the Upper Awash River basin

dc.contributor.authorTola, S.Y.
dc.contributor.authorShetty, A.
dc.date.accessioned2026-02-04T12:26:22Z
dc.date.issued2023
dc.description.abstractExtreme hydroclimatic variability in a changing climate and the possible causes of extreme hydrological variability are essential for effectively mitigating floods. The study aims to investigate the variability of extreme hydroclimatic conditions and the relationship between anomalies in extreme local precipitation, ENSO indicators (Southern Oscillation index (SOI), Niño 3.4, and multivariate ENSO index (MEI)), and extreme flow indices in the Upper Awash River basin, Ethiopia. The analysis used standardized anomaly index and coefficient of variation statistics to examine variability, the modified Mann-Kendall and Pettitt tests for trend and change point analysis, and Spearman’s correlation test to explore relationships. The study revealed that the basin-wise extreme precipitation indices had less variability but higher variability spatially, while the extreme flow indices showed high variability. Furthermore, the basin experienced extreme wet to normal wet conditions in the 1990s compared to the 2000s. The maximum temperature increased significantly, while the minimum temperature decreased significantly (except at a few northwest stations), with a considerable shift in the 1990s and 2000s. Anomalies, extreme to normal wet conditions, and a decrease in extreme precipitation were consistent with the extreme flow at the basin outlet, Hombole station. However, the extreme flow indices at Melka Kunture increased significantly and shifted upward (2003/2005), and the anomalies in extremely wet and very wet precipitation in the northwest were possibly responsible for this change. The study also revealed that the annual wet and very wet days of precipitation strongly affected the extreme flow in the basin. The effect of annual wet day precipitation, annual maximum precipitation, and ENSO anomalies on extreme flow at the Hombole was significant. These findings enhance the understanding of extreme hydroclimatic variability and prospective flood predictability and aid flood risk management. © 2023, The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature.
dc.identifier.citationTheoretical and Applied Climatology, 2023, 153, 46115, pp. 1117-1137
dc.identifier.issn0177798X
dc.identifier.urihttps://doi.org/10.1007/s00704-023-04510-4
dc.identifier.urihttps://idr.nitk.ac.in/handle/123456789/21796
dc.publisherSpringer
dc.subjectclimate conditions
dc.subjectclimate variation
dc.subjectEl Nino-Southern Oscillation
dc.subjectextreme event
dc.subjectglobal climate
dc.subjectprecipitation (climatology)
dc.subjectriver basin
dc.subjectAwash Basin
dc.subjectEthiopia
dc.titleExtreme hydroclimatic variability and impact of local and global climate system anomalies on extreme flow in the Upper Awash River basin

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