Please use this identifier to cite or link to this item: http://197.159.135.214/jspui/handle/123456789/573
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dc.contributor.authorBoko, Boubacar Abdou-
dc.contributor.authorKonaté, Moussa-
dc.contributor.authorYalo, Nicaise-
dc.contributor.authorBerg, Steven J.-
dc.contributor.authorErler, Andre R.-
dc.contributor.authorBazié, Pibgnina-
dc.contributor.authorHwang, Hyoun-Tae-
dc.contributor.authorSeidou, Ousmane-
dc.contributor.authorNiandou, Albachir Seydou-
dc.contributor.authorSchimmel, Keith-
dc.contributor.authorSudicky, Edward A.-
dc.date.accessioned2022-12-15T10:02:37Z-
dc.date.available2022-12-15T10:02:37Z-
dc.date.issued2020-
dc.identifier.otherdoi:10.3390/w12020364-
dc.identifier.urihttp://197.159.135.214/jspui/handle/123456789/573-
dc.descriptionResearch Articleen_US
dc.description.abstractThis study evaluates the impact of climate change on water resources in a large, semi-arid urban watershed located in the Niamey Republic of Niger, West Africa. The watershed was modeled using the fully integrated surface–subsurface HydroGeoSphere model at a high spatial resolution. Historical (1980–2005) and projected (2020–2050) climate scenarios, derived from the outputs of three regional climate models (RCMs) under the regional climate projection (RCP) 4.5 scenario, were statistically downscaled using the multiscale quantile mapping bias correction method. Results show that the bias correction method is optimum at daily and monthly scales, and increased RCM resolution does not improve the performance of the model. The three RCMs predicted increases of up to 1.6% in annual rainfall and of 1.58 C for mean annual temperatures between the historical and projected periods. The durations of the minimum environmental flow (MEF) conditions, required to supply drinking and agricultural water, were found to be sensitive to changes in runo resulting from climate change. MEF occurrences and durations are likely to be greater from 2020–2030, and then they will be reduced for the 2030–2050 statistical periods. All three RCMs consistently project a rise in groundwater table of more than 10 m in topographically high zones, where the groundwater table is deep, and an increase of 2 m in the shallow groundwater table.en_US
dc.language.isoenen_US
dc.publisherMDPIen_US
dc.subjectclimate changeen_US
dc.subjectintegrated hydrological modelen_US
dc.subjectsemi-ariden_US
dc.subjectimpactsen_US
dc.titleHigh-Resolution, Integrated Hydrological Modeling of Climate Change Impacts on a Semi-Arid Urban Watershed in Niamey, Nigeren_US
dc.typeArticleen_US
Appears in Collections:Climate Change and Water Resources

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