Titlebook: Nile River Basin; Ecohydrological Chal Assefa M. Melesse,Wossenu Abtew,Shimelis G. Setegn Book 2014 Springer International Publishing Switz

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Ayele Almaw Fenta,Tom Rientjes,Alemseged Tamiru Haile,Paolo Reggiani

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Satellite Rainfall Products and Their Reliability in the Blue Nile Basins a single peak in Lake Tana, Gilgel Abbay, and Jemma subbasins and double peaks in Belles, Dabus, and Muger subbasins. Maximum rain rate occurs in the morning (Gilgel Abbay, Dabus, and Jemma), afternoon (Belles, Beshilo, and Muger), and evening (Lake Tana and along the river gorges). Results of thi

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Africa-Wide Monitoring of Small Surface Water Bodies Using Multisource Satellite Data: A Monitoring ed gauge data demonstrated the ability of the model to capture both the spatial patterns and seasonal variations. Modeled scaled estimates captured up to 60 % of the observed gauge variability with a mean root-mean-square error (RMSE) of 22 %. The data on relative water level, precipitation, and eva

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Soil Erosion and Discharge in the Blue Nile Basin: Trends and Challenges 40-year periods as a result of the increase in degraded soils. Sediment loads appeared to have increased many times more, but this needs to be further validated as data availability is limited. In general, the results indicate that rehabilitating the degraded and bare areas by planting permanent ve

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Modeling Sediment Dynamics: Effect of Land Use, Topography, and Land Management in the Wami-Ruvu Basse/cover data to define crop/plant growth and tillage practices. Runoff also varied with soil type in all four watersheds. The highest and lowest total average annual soil loss rate was estimated in Mfizigo Juu, 45.09 kg/m. and Kibungo chini, 0.45 kg/m., respectively. The cultivated land contributed

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Assessment of Soil Erosion in the Blue Nile Basinge ditches has made a clear picture that ditches serve as both a source of erosion and a sediment transport channel for the soil eroded from the inter-ditch areas. The changes in depth and width of ditches constructed on moderate to steep slopes vary between 8 and 20 mm, and 20 and 30 mm during two

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Hydro-Epidemiology of the Nile Basin: Understanding the Complex Linkages Between Water and Infectiouin. Our synthesis of the literature emphasizes the importance of integrating public health concerns into the planning of new water development projects in the Nile basin and also highlights the potential for utilizing the underlying hydro-epidemiological relationships to enhance mapping and forecast

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Monitoring State of Biomass Recovery in the Blue Nile Basin Using Image-Based Disturbance Indexon campaigns. The DI maps are validated through field visits to 19 selected sites and inventory data obtained from the World Food Program (WFP) over five sites. The results showed that the largest expansion of plantations has taken place in five subbasins and is between 6 and 8.5 % of the subbasin a