Your search found 7 records
1 Sutcliffe, J. V.; Parks, Y. P. 1999. The hydrology of the Nile. Wallingford, UK: International Association of Hydrological Sciences (IAHS). xi, 179p. (IAHS special publication 5)
(Location: IWMI-HQ Call no: 551.483 G232 SUT Record No: H024430)
2 Beadle, L. C. 1974. The inland waters of tropical Africa: An introduction to tropical limnology. London, UK: Longman. 365p.
(Location: IWMI-HQ Call no: 551.48 G100 BEA Record No: H039368)
3 Rugumayo, A.; Kibera, G. 2004. Sustainable groundwater supply: A case study of Western Uganda. In Herath, S.; Pathirana, A.; Weerakoon, S. B. (Eds.). Proceedings of the International Conference on Sustainable Water Resources Management in the Changing Environment of the Monsoon Region. Bandaranaika Memorial International Conference Hall, Colombo, Sri Lanka, 17-19 November 2004. Vol.II. Colombo, Sri Lanka: National Water Resources Secretariat. pp.604-612.
(Location: IWMI-HQ Call no: 333.91 G000 HER Record No: H039550)
4 Benon, Z. T.; McCartney, Matthew. 2008. Evaluation of the water budgets of the equatorial lakes of the White Nile. Paper presented at the International Nile Basin Development Forum, Khartoum, Sudan, 3-5 November 2008. 15p.
(Location: IWMI HQ Call no: e-copy only Record No: H041834)
(0.27 MB)
5 Dumont, H. J. (Ed.) 2009. The Nile: origin, environments, limnology and human use. New York, NY, USA: Springer. 818p. (Monographiae Biologicae, Vol. 89)
(Location: IWMI HQ Call no: 577.64 G100 DUM Record No: H042456)
6 Nicol, Alan; Odinga, W. 2016. IWRM [Integrated Water Resources Management] in Uganda - progress after decades of implementation. Water Alternatives, 9(3):627-643. (Special issue: Flows and Practices: The Politics of Integrated Water Resources Management (IWRM) in southern Africa).
(Location: IWMI HQ Call no: e-copy only Record No: H047822)
(0.90 MB) (920 KB)
Uganda lies almost wholly within the Nile Basin and is a country characterised as well-endowed with water resources. Receiving considerable inflows of aid since the early 1990s, some of this aid emerging after the 1992 Earth Summit in Rio de Janeiro enabled the country to begin a process of Integrated Water Resources Management (IWRM), taking the lead from Chapter 18 of Agenda 21. With a focus on more comprehensively managing the country’s critical water endowment amidst growing pressure on the resource, bilateral technical assistance and financial support played a large part in backstopping these national efforts. Nevertheless, in spite of this support and government backing, some two decades later implementation on the ground remains thin and the exercise of IWRM in practice is limited. This paper examines the Ugandan IWRM experience and identifies complex political-economy issues lying at the heart of current challenges. It argues that rarely is there likely to be an easy fix to sustainable financing and suggests the need for stronger citizen engagement and buy-in to the wider logic of IWRM to support longer-term effectiveness and sustainability.
(Location: IWMI HQ Call no: e-copy only Record No: H048049)
(3.24 MB)
Although the use of the Gravity Recovery and Climate Experiment (GRACE) satellites to monitor groundwater storage changes has become commonplace, our evaluation suggests that careful processing of the GRACE data is necessary to extract a representative signal especially in regions with significant surface water storage (i.e., lakes/reservoirs). In our study, we use cautiously processed data sets, including GRACE, lake altimetry, and model soil moisture, to reduce scaling factor bias and compare GRACE-derived groundwater storage changes to in situ groundwater observations over parts of East Africa. Over the period 2007–2010, a strong correlation between in situ groundwater storage changes and GRACE groundwater estimates (Spearman's = 0.6) is found. Piecewise trend analyses for the GRACE groundwater estimates reveal significant negative storage changes that are attributed to groundwater use and climate variability. Further analysis comparing groundwater and satellite precipitation data sets permits identification of regional groundwater characterization. For example, our results identify potentially permeable and/or shallow groundwater systems underlying Tanzania and deep and/or less permeable groundwater systems underlying the Upper Nile basin. Regional groundwater behaviors in the semiarid regions of Northern Kenya are attributed to hydraulic connections to recharge zones outside the subbasin boundary. Our results prove the utility of applying GRACE in monitoring groundwater resources in hydrologically complex regions that are undersampled and where policies limit data accessibility.
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