Organization for the Development of the Senegal River
Geolocation: | 16° 30' 52.3307", -14° 44' 33.8392" |
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Total Population | 5,597,6005,597,600,000,000 millionmillion |
Total Area | 434,518434,518 km² 167,767.4 mi² km2 |
Climate Descriptors | Moist tropical (Köppen A-type), Semi-arid/steppe (Köppen B-type), Moist, Monsoon |
Predominent Land Use Descriptors | agricultural- cropland and pasture, rangeland |
Important Uses of Water | Agriculture or Irrigation, Hydropower Generation |
Water Features: | Senegal River |
Water Projects: | Manantali Dam |
Contents
Summary
The Senegal River, the second-largest river in Western Africa, originates in the Fouta Djallon Mountains of Guinea where its three main tributaries, the Bafing, Bakoye, and Faleme contribute 80% of the river's flow. After originating in Guinea, the Senegal River then travels 1,800 km crossing Mali, Mauritania and Senegal on its way to the Atlantic Ocean. [1]Following the independence of the basin countries, tension remained in the region due to the instability of the political powers and the influence of neo-colonial states such as the United States and the Soviet Union. Throughout the turmoil following World War II into the 1970s, the Senegal River continued to be a common link between the basin countries. There was a desire between them to cooperate in the management of the basin so that all countries would benefit from its development. This aspiration has been carried into the twenty-first century as Guinea, Mali, Mauritania and Senegal work cooperatively toward more effective basin management. The history of cooperation over this river basin has led to numerous multilateral agreements, projects and organizations over the last 25 years. The Manantali Dam has been working at full capacity since May 2003 providing each of the basin countries with electricity based on the amount the invested in the dam project.The Senegal River Charter, signed in 2002, sets the principles and procedures for allocating water between the various use sectors, defines procedures for the examination and acceptance of new water use projects, determines regulations for environmental preservation and protection and defines the framework and procedures for water user participation in resource management decision-making bodies.
Natural, Historic, Economic, Regional, and Political Framework
Image 1. Map of the Senegal River Basin.[2]
Background
The Senegal River, the second-largest river in Western Africa, originates in the Fouta Djallon Mountains of Guinea where its three main tributaries, the Bafing, Bakoye, and Faleme contribute 80% of the river's flow. After originating in Guinea, the Senegal River then travels 1,800 km crossing Mali, Mauritania and Senegal on its way to the Atlantic Ocean.
Following the independence of the basin countries, tension remained in the region due to the instability of the political powers and the influence of neo-colonial states such as the United States and the Soviet Union. Throughout the turmoil following World War II into the 1970s, the Senegal River continued to be a common link between the basin countries. There was a desire between them to cooperate in the management of the basin so that all countries would benefit from its development. This aspiration has been carried into the twenty-first century as Guinea, Mali, Mauritania and Senegal work cooperatively toward more effective basin management.
The river is a key resource for all three countries. Large herds of cattle, camels, goats and sheep migrate season to season across these borders and herders rely on this water source to sustain their herds. The basin region receives only an average of 660mm of rainfall per year, therefore the Senegal river waters represent the key to agriculture in the region. On the left bank, the surface area of community-based irrigated fields grew from 20 hectares in 1974 to 7,335 hectares in 1983 and 12,978 hectares in 1986. After agriculture, fishing is the largest economic activity in the region. Other river based economic activities include sugar cane production, rice framing and, to a lesser extent, mining,
Two dams, Manantali and Diama, were built in 1986 and 1988, respectively, in order to provide fresh water for agriculture and municipal uses and, in the case of the Manantali Dam, eventually to produce hydroelectric power for the region. These two dams were part of an economic growth strategy for the region that would reduce the investment risk and reduce poverty by increasing income-generating activities. The Manantali Dam was put on line in 2002 and is now supplying the three basin countries with 547 gwh/yr.
Analysis, Synthesis, and Insight
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Learn moreASI:Organization for the Development of the Senegal River: Insights from the Transboundary Freshwater Dispute Database
Contributed by: Aaron T. Wolf, Joshua T. Newton, Matthew Pritchard (last edit: 12 February 2013)
- ^ Product of the Transboundary Freshwater Dispute Database, Department of Geosciences, Oregon State University. Additional information about the TFDD can be found at: http://www.transboundarywaters.orst.edu/research/case_studies/OMVS_New.htm
- ^ Product of the Transboundary Freshwater Dispute Database, Department of Geosciences, Oregon State University. Additional information about the TFDD can be found at:http://www.transboundarywaters.orst.edu/research/case_studies/OMVS_New.htm