Analysis of drought and wet-events using swsi-based severity-duration-frequency (SDF) curves for the upper Tana River basin, Kenya

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dc.contributor.author Wambua, Raphael M.
dc.contributor.author Mutua, Benedict M.
dc.contributor.author Raude, James M.
dc.date.accessioned 2022-10-24T08:52:17Z
dc.date.available 2022-10-24T08:52:17Z
dc.date.issued 2018-06-12
dc.identifier.citation Hydrology, Volume 6, Issue 2, Pages: 43-52 2018 en_US
dc.identifier.issn 2306-5338
dc.identifier.uri https://membership.sciencepublishinggroup.com/journal/paperinfo?journalid=267&doi=10.11648/j.hyd.20180602.11
dc.identifier.uri http://repository.seku.ac.ke/handle/123456789/6888
dc.description doi: 10.11648/j.hyd.20180602.11 en_US
dc.description.abstract Drought and wet-event patterns in the Upper Tana River basin have significantly been changing due to variation of climatic and human-induced factors. This paper presents the analysis of drought and wet-events using Severity-Duration-Frequency (SDF) curves for the Upper Tana River basin, Kenya based on Surface Water Supply Index (SWSI). The extreme value EV1 (Gumbel) frequency distribution function was used to formulate SDF curves. The developed SDF curves were used to develop isoseverity maps for the basin. From the results, the event-probability show that likelihood of drought events increased linearly with increase in magnitude of SWSI while the return period of drought events increased exponentially with decrease in magnitude of SWSI. The findings show that the probability and magnitude, the return period and magnitude of drought have linear and exponential regression coefficients of 0.984 and 0.980 respectively. On the other hand the probability of wet-period events decreased linearly with increase in magnitude of SWSI while the return period of the events increased exponentially with increase in magnitude of SWSI with regression coefficients of the linear and exponential functions of 0.804 and 0.881 respectively. This indicates that both the drought and wet-events probability and magnitude, and the return period and magnitude have a strong correlation. Spatially, it was found that generally the river basin exhibit an increasing pattern in cumulative SWSI in south-eastern areas than the north-eastern and generally a more increase in extreme wet-events than droughts in the basin. The developed (SDF) curves are critical for design of hydrologic, hydraulic and water resources supply systems while the spatial event-patterns can be incorporated in prioritized mitigation of extreme events. en_US
dc.language.iso en en_US
dc.publisher MDPI en_US
dc.subject SDF Curves en_US
dc.subject Drought en_US
dc.subject Wet-Event en_US
dc.subject SWSI en_US
dc.subject Isoseverity en_US
dc.subject Return Period en_US
dc.subject Event-Probability en_US
dc.subject Upper Tana River Basin en_US
dc.title Analysis of drought and wet-events using swsi-based severity-duration-frequency (SDF) curves for the upper Tana River basin, Kenya en_US
dc.type Article en_US


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