Articles | Volume 21, issue 6
https://doi.org/10.5194/hess-21-3145-2017
https://doi.org/10.5194/hess-21-3145-2017
Research article
 | 
29 Jun 2017
Research article |  | 29 Jun 2017

Modeling the water budget of the Upper Blue Nile basin using the JGrass-NewAge model system and satellite data

Wuletawu Abera, Giuseppe Formetta, Luca Brocca, and Riccardo Rigon

Related authors

The design, deployment, and testing of kriging models in GEOframe with SIK-0.9.8
Marialaura Bancheri, Francesco Serafin, Michele Bottazzi, Wuletawu Abera, Giuseppe Formetta, and Riccardo Rigon
Geosci. Model Dev., 11, 2189–2207, https://doi.org/10.5194/gmd-11-2189-2018,https://doi.org/10.5194/gmd-11-2189-2018, 2018
Short summary

Related subject area

Subject: Water Resources Management | Techniques and Approaches: Modelling approaches
Impact of reservoir evaporation on future water availability in north-eastern Brazil: a multi-scenario assessment
Gláuber Pontes Rodrigues, Arlena Brosinsky, Ítalo Sampaio Rodrigues, George Leite Mamede, and José Carlos de Araújo
Hydrol. Earth Syst. Sci., 28, 3243–3260, https://doi.org/10.5194/hess-28-3243-2024,https://doi.org/10.5194/hess-28-3243-2024, 2024
Short summary
How economically and environmentally viable are multiple dams in the upper Cauvery Basin, India? A hydro-economic analysis using a landscape-based hydrological model
Anjana Ekka, Yong Jiang, Saket Pande, and Pieter van der Zaag
Hydrol. Earth Syst. Sci., 28, 3219–3241, https://doi.org/10.5194/hess-28-3219-2024,https://doi.org/10.5194/hess-28-3219-2024, 2024
Short summary
Leveraging a novel hybrid ensemble and optimal interpolation approach for enhanced streamflow and flood prediction
Mohamad El Gharamti, Arezoo Rafieeinasab, and James L. McCreight
Hydrol. Earth Syst. Sci., 28, 3133–3159, https://doi.org/10.5194/hess-28-3133-2024,https://doi.org/10.5194/hess-28-3133-2024, 2024
Short summary
A generalised ecohydrological landscape classification for assessing ecosystem risk in Australia due to an altering water regime
Alexander Herr, Linda E. Merrin, Patrick J. Mitchell, Anthony P. O'Grady, Kate L. Holland, Richard E. Mount, David A. Post, Chris R. Pavey, and Ashley D. Sparrow
Hydrol. Earth Syst. Sci., 28, 1957–1979, https://doi.org/10.5194/hess-28-1957-2024,https://doi.org/10.5194/hess-28-1957-2024, 2024
Short summary
Process-based three-layer synergistic optimal-allocation model for complex water resource systems considering reclaimed water
Jing Liu, Yue-Ping Xu, Wei Zhang, Shiwu Wang, and Siwei Chen
Hydrol. Earth Syst. Sci., 28, 1325–1350, https://doi.org/10.5194/hess-28-1325-2024,https://doi.org/10.5194/hess-28-1325-2024, 2024
Short summary

Cited articles

Abera, W., Formetta, G., Brocca, L., and Rigon, R.: Complimentary material and data, https://doi.org/10.5281/zenodo.264004, 2017.
Abera, W., Antonello, A., Franceschi, S., Formetta, G., and Rigon, R.: The uDig Spatial Toolbox for hydro-geomorphic analysis, British Society for Geomorphology, London, UK, in: geomorphological techniques (online Edn.), edited by: Clarke, L. E. and Nield, J. M., 2014.
Abera, W., Brocca, L., and Rigon, R.: Comparative evaluation of different satellite rainfall estimation products and bias correction in the Upper Blue Nile (UBN) basin, Atmos. Res., 178, 471–483, 2016.
Abera, W., Formetta, G., Borga, M., and Rigon, R.: Estimating the water budget components and their variability in a pre-alpine basin with JGrass-NewAGE, Adv. Water Resour., 104, 37–54, 2017.
Abtew, W., Melesse, A. M., and Dessalegne, T.: Spatial, inter and intra-annual variability of the Upper Blue Nile Basin rainfall, Hydrol. Process., 23, 3075–3082, 2009.
Download
Short summary
This study documents a state-of-the-art estimation of the water budget (rainfall, evapotranspiration, discharge, and soil and groundwater storage) components for the Upper Blue Nile river. The budget uses various JGrass-NewAGE components, satellite data and all ground measurements available. The analysis shows that precipitation of the basin is 1360 ± 230 mm per year. Evapotranspiration accounts for 56 %, runoff is 33 %, and storage varies from minus 10 % to plus 17 % of the annual water budget.