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The discharge of the Nile River is highly dependent on the flow generated in the highlands of Ethiopia. However, little is known about the local (i.e. small scale) watershed hydrological response, due in part to a lack of long duration, continuous hydrological data. The goal of this paper was to ...


Collick, A.S.Easton, Z.M.Ashagrie, T.Biruk, B.Tilahun, S.Adgo, E.Awulachew, Seleshi BekeleZeleke, G.Steenhuis, Tammo S.[A simple semi-distributed water balance model for the Ethiopian highlands]A simple semi-distributed water balance model for the Ethiopian highlands

The discharge of the Nile River is highly dependent on the flow generated in the highlands of Ethiopia. However, little is known about the local (i.e. small scale) watershed hydrological response, due in part to a lack of long duration, continuous hydrological data. The goal of this paper was to ...


Collick, A.S.Easton, Z.M.Ashagrie, T.Biruk, B.Tilahun, S.Adgo, E.Awulachew, Seleshi BekeleZeleke, G.Steenhuis, Tammo S.[A simple semi-distributed water balance model for the Ethiopian highlands]A simple semi-distributed water balance model for the Ethiopian highlands

Watershed scale hydrological and biogeochemical models rely on the correct spatial-temporal prediction of processes governing water and contaminant movement. The Soil and Water Assessment Tool (SWAT) model, one of the most commonly used watershed scale models, uses the popular curve number (CN) m...


White, E.D.Easton, Z.M.Fuka, D.R.Collick, A.S.Adgo, E.McCartney, Matthew P.Awulachew, Seleshi BekeleSelassie, Y.G.Steenhuis, Tammo S.[Development and application of a physically based landscape water balance in the SWAT model]Development and application of a physically based landscape water balance in the SWAT model

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