Your search found 4 records
1 Awulachew, Seleshi Bekele; Tenaw, M.; Steenhuis, T.; Easton, Z.; Ahmed, A.; Bashar, K. E.; Hailesellassie, A. 2008. Impact of watershed interventions on runoff and sedimentation in Gumera Watershed. In Humphreys, E.; Bayot, R. S.; van Brakel, M.; Gichuki, F.; Svendsen, M.; Wester, P.; Huber-Lee, A.; Cook, S. Douthwaite, B.; Hoanh, Chu Thai; Johnson, N.; Nguyen-Khoa, Sophie; Vidal, A.; MacIntyre, I.; MacIntyre, R. (Eds.). Fighting poverty through sustainable water use: proceedings of the CGIAR Challenge Program on Water and Food, 2nd International Forum on Water and Food, Addis Ababa, Ethiopia, 10-14 November 2008. Vol.1. Keynotes; Cross-cutting topics. Colombo, Sri Lanka: CGIAR Challenge Program on Water and Food. pp.109-113.
River basins ; Flow ; Simulation models ; Watershed management ; Runoff ; Sedimentation ; Erosion ; Soil loss ; Soil degradation / Ethiopia / Sudan / Gumera Watershed / Abbay-Blue Nile River Basin
(Location: IWMI HQ Call no: IWMI 333.91 G000 HUM Record No: H041752)
http://cgspace.cgiar.org/bitstream/handle/10568/3706/IFWF2_proceedings_Volume%20I.pdf?sequence=1
https://vlibrary.iwmi.org/pdf/H041752.pdf
https://vlibrary.iwmi.org/pdf/H041752.pdf
(7.964MB)
2 Steenhuis, T. S.; Taylor, J.; Easton, Z.; Collick, A.; van de Giesen, N.; Liebe, J.; Ahmed, A. A.; Andreini, Marc. 2009. Rainfall-discharge relationships for monsoonal climates. In Awulachew, Seleshi Bekele; Erkossa, Teklu; Smakhtin, Vladimir; Fernando, Ashra (Comps.). Improved water and land management in the Ethiopian highlands: its impact on downstream stakeholders dependent on the Blue Nile. Intermediate Results Dissemination Workshop held at the International Livestock Research Institute (ILRI), Addis Ababa, Ethiopia, 5-6 February 2009. Colombo, Sri Lanka: International Water Management Institute (IWMI). pp.141-151.
Runoff ; Water balance ; Models ; River basins / Africa / Ethiopia / Blue Nile River Basin / Abay Blue Nile basin / Volta Basin
(Location: IWMI HQ Call no: IWMI 333.9162 G100 AWU Record No: H042514)
(0.60 MB)
Methods for estimating runoff that have been developed for temperate climates may not be suitable for use in the monsoonal climates of Africa, where there is a distinct dry season during which soils dry out to a considerable depth. This has a distinct effect on runoff generation that is not captured by “the temperate climate” models. The scope of this tool is to develop a simple water balance method for predicting river discharge. Water balance models have been shown to better predict river discharge in regions with monsoonal climates than alternative methods based on the United States Department of Agriculture-Soil Conservation Service (USDA-SCS) curve number. The latter is an empirical-based model developed in the USA that does not apply to monsoonal climates with distinct dry and wet periods.
3 Steenhuis, T.; Taylor, J.; Collick, A.; van de Giesen, N.; Liebe, J.; Andreini, Marc; Easton, Z.. 2009. Rainfall-discharge relationships for monsoonal climates. In Andreini, Marc; Schuetz, Tonya; Harrington, Larry (Eds.). Small reservoirs toolkit, theme 2 b: hydrology and physical measures of performance. Colombo, Sri Lanka: CGIAR Challenge Program on Water and Food (CPWF); Colombo, Sri Lanka: International Water Management Institute (IWMI); Brasilia, DF, Brasil: Brazilian Agricultural Research Corporation (Embrapa Cerrados Center); Harare, Zimbabwe: University of Zimbabwe (UZ); Accra, Ghana: Ghana Water Research Institution (WRI); Delft, The Netherlands: Delft University of Technology (TUD); Stockholm, Sweden: Stockholm Environment Institute (SEI); Marseille, France: Institut de Recherche pour le Developpement (IRD); Bonn, Germany: Center for Development Research, University of Bonn; Ithaca, NY, USA: Cornell University. 10p.
Rivers ; Discharges ; Water balance ; Simulation models ; Watersheds ; Climate ; Rain ; Evapotranspiration / Africa / Abay Blue Nile / Volta Basin
(Location: IWMI HQ Call no: e-copy only Record No: H042665)
Methods for estimating runoff that have been developed for temperate climates may not be suitable for use in the monsoonal climates of Africa, where there is a distinct dry season in which soils dry out to a considerable depth. Water balance models have been shown to better predict river discharge in regions with monsoonal climates than alternative methods based on rainfall intensity, or on the USDA-SCS curve number. This tool can be used to develop a simple water balance model for predicting river discharge.
4 Awulachew, Seleshi Bekele; Tenaw, M.; Steenhuis, T.; Easton, Z.; Ahmed, A.; Bashar, K. E. 2008. Blue Nile flow, sediment and impact of watershed interventions: case of Gumera Watershed. Paper presented at the Second International Forum on Water and Food, Addis Ababa, Ethiopia, 10-13 November 2008. 8p.
Watershed management ; Erosion ; Sedimentation ; Runoff ; Models ; Flow ; River basins / Ethiopia / Gumera Watershed / Abbay-Blue Nile Basin
(Location: IWMI HQ Call no: e-copy only Record No: H043010)
(0.49 MB) (0.49 MB)
High population pressure, inappropriate agricultural policies, improper land-use planning, over-dependency on agriculture as source of livelihood and extreme dependence on natural resources are inducing deforestation, overgrazing, expansion of agriculture to marginal lands and steep slopes, declining agricultural productivity and resource-use conflicts in many parts of Blue Nile. Increased land degradation from poor agricultural practices and erosion results in increased siltation and the reduced water quality in the river basin. The rainfall, runoff and sediment are highly variable both in time and space. Poor water and land management upstream severely affect runoff characteristics and the quality of water reaching downstream. The result is a downward spiral of poverty and food insecurity for millions of people both within the upper catchment and downstream across international borders. Quantification of the erosion, sedimentation processes and evaluation of impacts of interventions are difficult tasks. This paper schematizes the Blue Nile Basin (BNB) at various spatial levels as micro watershed, watershed, sub-basin to basin. It considers a particular watershed to model runoff, sediment and impact of watershed intervention. The result shows that runoff can be reasonably simulated with calibration of R2=0.87 and validation of result of 0.82, and comparable sediment modelling results. The study also demonstrates, by undertaking spatial analysis using topographic, soil and land use parameters it is possible to identify the high sediment risk sub-watersheds. Impact of typical watershed intervention using various widths of vegetative filter and application on high erosion risk watersheds show reduction of sediment yield from 52% to 74%
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