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High-Resolution, Integrated Hydrological Modeling of Climate Change Impacts on a Semi-Arid Urban Watershed in Niamey, Niger

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dc.contributor.author Boko, Boubacar Abdou
dc.contributor.author Konaté, Moussa
dc.contributor.author Yalo, Nicaise
dc.contributor.author Berg, Steven J.
dc.contributor.author Erler, Andre R.
dc.contributor.author Bazié, Pibgnina
dc.contributor.author Hwang, Hyoun-Tae
dc.contributor.author Seidou, Ousmane
dc.contributor.author Niandou, Albachir Seydou
dc.contributor.author Schimmel, Keith
dc.contributor.author Sudicky, Edward A.
dc.date.accessioned 2022-12-15T10:02:37Z
dc.date.available 2022-12-15T10:02:37Z
dc.date.issued 2020
dc.identifier.other doi:10.3390/w12020364
dc.identifier.uri http://197.159.135.214/jspui/handle/123456789/573
dc.description Research Article en_US
dc.description.abstract This 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.iso en en_US
dc.publisher MDPI en_US
dc.subject climate change en_US
dc.subject integrated hydrological model en_US
dc.subject semi-arid en_US
dc.subject impacts en_US
dc.title High-Resolution, Integrated Hydrological Modeling of Climate Change Impacts on a Semi-Arid Urban Watershed in Niamey, Niger en_US
dc.type Article en_US


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