Thesis Open Access
Misganaw Gonbis
<?xml version='1.0' encoding='utf-8'?> <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"> <dc:creator>Misganaw Gonbis</dc:creator> <dc:date>2021-08-25</dc:date> <dc:description>This study is conducted Northeastern upper Jemma River catchment, which is located in the Abay Basin. Though groundwater serves as the main safe drinking water supply source in the study area, there were no detail study in the recharge amount and distribution. The main objective of this thesis is to quantify the amount and spatial distribution of groundwater recharge over study catchment using the WetSpass model. As input to the model: -precipitation, potential evapotranspiration, temperature, and wind speed were estimated using data collected from meteorological stations located within and nearby the Catchment, the physical environmental data including land use, soil type, and groundwater depth are evaluated from field observation and existing maps. Slope and topography were generated from DEM data. Input data for the model were prepared in the form of grid maps using 100m grid size and the parameter attribute tables were adjusted to represent the catchment condition using scientific literature. The results of the model showed that the long-term average annual rainfall of 1118 mm was partitioned to 271 mm (24%) of surface runoff, 612 mm (55%) of evapotranspiration, and 235 mm (21%) of recharge. The model output is found to be comparable with recharge estimation in nearby areas having similar climatic and physical characteristics. Finally, the study result provides baseline information for water resource experts and policymakers of the region for further investigation of water resources, design, sustainable developmental activities, and for land use managing and planning purposes. It is concluded that the groundwater recharge estimation using the WetSpass model is reasonable and useful for quantification of annual groundwater recharge with spatial and seasonal variation.</dc:description> <dc:identifier>https://nadre.ethernet.edu.et/record/20940</dc:identifier> <dc:identifier>10.20372/nadre/20940</dc:identifier> <dc:language>eng</dc:language> <dc:relation>doi:10.20372/nadre/20939</dc:relation> <dc:relation>url:https://nadre.ethernet.edu.et/communities/aastuet</dc:relation> <dc:relation>url:https://nadre.ethernet.edu.et/communities/nadre</dc:relation> <dc:rights>info:eu-repo/semantics/openAccess</dc:rights> <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights> <dc:subject>Groundwater Recharge, WetSpass, Northeastern Upper Jemma, Abay Basin</dc:subject> <dc:title>Recharge Estimation Using WetSpass Model in Northeastern Upper Jemma River Catchment, Abay Basin, Ethiopia.</dc:title> <dc:type>info:eu-repo/semantics/doctoralThesis</dc:type> <dc:type>publication-thesis</dc:type> </oai_dc:dc>
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