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dc.contributor.authorGadissa, Takele
dc.contributor.authorNyadawa, Maurice
dc.contributor.authorBehulu, Fiseha
dc.contributor.authorMutua, Benedict
dc.date.accessioned2020-08-20T09:19:38Z
dc.date.available2020-08-20T09:19:38Z
dc.date.issued2019-11-01
dc.identifier.urihttp://ir.jooust.ac.ke:8080/xmlui/handle/123456789/8826
dc.description.abstractThis chapter describes the impact of climate change on available water resources under increasing demand in Central Rift Valley Basin. The study used the ensemble mean of five regional climate models (RCMs) under CORDEX—Africa. Two Representative Concentration Pathways, RCP4.5 and RCP8.5, for current (1985–2016) and scenario period (2041–2070) were considered. The study has revealed that maximum temperature will increase on average by 1.73°C under RCP4.5 to 2.36°C under RCP8.5. Minimum temperature will increase by 2.16°C under RCP4.5 to 3.07°C under RCP8.5. On average, precipitation decreases by 7.97% and − 2.55% under RCP4.5 and RCP8.5, respectively. Moreover, the average streamflow of Meki River will change by − 10.4% and 0.5% under RCP4.5 and RCP8.5, respectively. However, the streamflow of Ketar River will decline by 18.8% and 3.4% on average under RCP4.5 and RCP8.5, respectively. Hence, the available water resources will not meet the projected demand in the scenario period.en_US
dc.language.isoenen_US
dc.publisherScienceDirecten_US
dc.subjectClimate changeen_US
dc.subjectDemanden_US
dc.subjectStream flowen_US
dc.subjectRCMsen_US
dc.subjectRCP4.5en_US
dc.subjectRCP8.5en_US
dc.titleChapter 13 - Assessment of Catchment Water Resources Availability Under Projected Climate Change Scenarios and Increased Demand in Central Rift Valley Basinen_US
dc.typeBook chapteren_US


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