Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/28070
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dc.contributor.authorKuti, Abayomi ibrahim-
dc.contributor.authorAnimashaun, Murtala-
dc.contributor.authorOlawale, Babatunde-
dc.contributor.authorAbdullahi, Suleiman-
dc.date.accessioned2024-05-07T09:09:35Z-
dc.date.available2024-05-07T09:09:35Z-
dc.date.issued2015-12-01-
dc.identifier.citationKuti I. A, ,Animashaun.M,, Olawale B.,& Abdullahi S.(2015).Trend Analysis of Hydro-meteorological Data for River Kaduna at Shiroro Dam Site, Niger State Nigeria. Journal of Scientific Research & Reports 8(5): 1-12, 2015;en_US
dc.identifier.issn2320-0227-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/28070-
dc.description.abstractVariation in the hydro-climatic variables of River Kaduna at Shiroro Dam site, Nigeria is linked to a number of climate change activities around the river. In view of this, the paper aims at examining the trend of stream flow, rainfall, temperature and evaporation. Monthly discharge, rainfall, temperature and evaporation records were obtained for a period of Thirty Three (33) years (1980- 2012). These variables were used to examine the trend of the area. Incremental/Reductional analysis was used to determine a positive and negative change with percentage hydro-climatic variables difference. Mann- Kendall test, Turning point test and Kendall’s Rank Correlation were also used to estimate the significance of the trend. The result of the Mann –Kendall shows that the month of September had a value of Zs equals -2.09 (greater thanen_US
dc.language.isoenen_US
dc.publisherJournal of Scientific Research and Reportsen_US
dc.relation.ispartofseriesJSRR_18331;8(5)-
dc.subjectClimate Changeen_US
dc.subjectTUrning Point Testen_US
dc.subjectKendall’s rank correlation testen_US
dc.subjectrend analysisen_US
dc.subjectShiroro Riveren_US
dc.titleTrend Analysis of Hydro-meteorological Data for River Kaduna at Shiroro Dam Site, Niger State Nigeriaen_US
dc.typeArticleen_US
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