Please use this identifier to cite or link to this item: http://197.159.135.214/jspui/handle/123456789/296
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dc.contributor.authorLarbi, Isaac-
dc.date.accessioned2021-05-19T10:14:47Z-
dc.date.available2021-05-19T10:14:47Z-
dc.date.issued2019-03-
dc.identifier.urihttp://197.159.135.214/jspui/handle/123456789/296-
dc.descriptionA Thesis submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Universite Abomey Calavi, Cotonou, Benin, in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Climate Change and Water Resourcesen_US
dc.description.abstractThis study assessed the impact of climate and land use/land cover (LULC) change on the water balance components in the Vea catchment, West Africa using the Soil and Water Assessment Tool (SWAT) model. The specific objectives of the study were to, (i) predict the changes in LULC of the Vea catchment based on different LULC change scenarios, (ii) investigate the impact of the Representative Concentration Pathways (RCP4.5) climate change scenario on rainfall, temperature and climate extremes in the future 2020-2049, and (iii) assess the impact of climate and LULC change scenarios on the water balance components. Data used for the study includes, observations (stations and satellite) climate data, Landsat images (1990, 2001, 2011 and 2016) for LULC mapping and prediction, Regional Climate Models (RCMs) and Statistical Downscaling Model- Decision Centric (SDSM-DC) for RCP4.5 scenario for historical and future (2020-2049) period for climate change impact assessment. The study found a decrease in natural vegetation due to cropland expansions over the past years, and a continuous decrease in forest/mixed vegetation and increase in cropland in the future 2025 under business-as-usual (BAU) scenario. The multi-model ensemble mean projected a warmer climate in the future (2020-2049) with a 1.3oC increase in mean annual temperature and a 4.2% increase in mean annual rainfall relative to the baseline (1981-2010) period. Surface runoff was found more sensitive to climate change (-42.7% changes) than land use change under BAU (+18.7 change) and afforestation scenarios (-19.6% change), followed by water yield which under climate change decreased by 43.8% compared to +18.4% and -15.7% changes under BAU and afforestation scenarios of land use change, respectively. The actual evapotranspiration was however found to be less sensitive to land use change (-2.7 and +0.6 % changes) than climate change (+9% changes).en_US
dc.description.sponsorshipThe Federal Ministry of Education and Research (BMBF)en_US
dc.language.isoenen_US
dc.publisherWASCALen_US
dc.subjectClimate extremesen_US
dc.subjectLand use changeen_US
dc.subjectRegional climate modelsen_US
dc.subjectSWAT modelen_US
dc.subjectVea catchmenten_US
dc.subjectWater balance componentsen_US
dc.titleAssessment of Climate and Land Use Change Impacts on the Water Balance Components in the Vea Catchment, West Africaen_US
dc.typeThesisen_US
Appears in Collections:Climate Change and Water Resources - Batch 1

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