World Library  
Flag as Inappropriate
Email this Article

Lake Chad

Article Id: WHEBN0000059314
Reproduction Date:

Title: Lake Chad  
Author: World Heritage Encyclopedia
Language: English
Subject: 2010 Sahel famine, Geography of Chad, Chad, Cameroon, Geography of Cameroon
Publisher: World Heritage Encyclopedia

Lake Chad

Lake Chad
Photograph taken by Apollo 7, October 1968
Map of lake and surrounding region
Lake type Endorheic
Primary inflows Chari River
Primary outflows Soro & Bodélé depressions
Basin countries Chad, Cameroon, Niger, Nigeria
Surface area 1,350 km2 (520 sq mi) (2005)[1]
Average depth 1.5 m[2]
Max. depth 11 m[3]
Water volume 72 km3 (17 cu mi).[3]
Shore length1 650 km
Surface elevation 278 to 286 metres (912 to 938 ft)
References [1]
1 Shore length is not a well-defined measure.

Lake Chad (French: lac Tchad) is a historically large, shallow, endorheic lake in Africa, the size of which has varied over the centuries. According to the Global Resource Information Database of the United Nations Environment Programme, it shrank as much as 95% from about 1963 to 1998, but "the 2007 (satellite) image shows significant improvement over previous years."[4] Lake Chad is economically important, providing water to more than 68 million people living in the four countries surrounding it (Chad, Cameroon, Niger, and Nigeria) on the edge of the Sahara Desert.[5] It is the largest lake in the Chad Basin.

Geography and hydrology

Lake Chad is located mainly in the far west of Chad, bordering on northeastern Nigeria. The Chari River, fed by its tributary the Logone, provides over 90% of Lake Chad's water, with a small amount coming from the Yobe River in Nigeria/Niger. Despite high levels of evaporation, the lake is fresh water. Over half of the lake's area is taken up by its many small islands (including Bogomerom archipelago), reedbeds and mud banks, and a belt of swampland across the middle divides the northern and southern halves while the shorelines are largely composed of marshes.

Because Lake Chad is very shallow—only 10.5 metres (34 ft) at its deepest—its area is particularly sensitive to small changes in average depth, and consequently it also shows seasonal fluctuations in size of about 1 m every year. Lake Chad has no apparent outlet, but its waters percolate into the Soro and Bodélé depressions. The climate is dry most of the year, with occasional rains from June to December.


Maximum extension of the Holocene "Lake Mega-Chad" (light blue area limited by a blue dotted line)
Lake Chad in a 2001 satellite image, with the actual lake in blue, and vegetation on top of the old lake bed in green. Above that, the changes from 1973 to 1997 are shown
The same changes marked more clearly on another map

Lake Chad gave its name to the country of Chad. The name Chad is a local word meaning "large expanse of water", in other words, a "lake".[6]

Lake Chad is the remnant of a former inland sea, paleolake Mega-Chad. At its largest, sometime before 5000 BC, Lake Mega-Chad was the largest of four Saharan paleolakes, and is estimated to have covered an area of 1,000,000 km2 (390,000 sq mi), larger than the Caspian Sea is today, and may have extended as far northeast as within 100 km (62 mi) of Faya-Largeau.[7] [8]

Lake Chad was first surveyed from shore by Europeans in 1823, and it was considered to be one of the largest lakes in the world then.[9] In 1851, a party including the German explorer Heinrich Barth carried a boat overland from Tripoli across the Sahara Desert by camel and made the first European waterborne survey.[10] British expedition leader James Richardson died just days before reaching the lake.

Lake Chad has shrunk considerably since the 1960s, when its shoreline had an elevation of about 286 metres (938 ft) above sea level[11] and it had an area of more than 26,000 square kilometres (10,000 sq mi), making its surface the fourth largest in Africa. An increased demand on the lake's water from the local population has likely accelerated its shrinkage over the past 40 years.[2]

The size of Lake Chad greatly varies seasonally with the flooding of the wetlands areas. In 1983, Lake Chad was reported to have covered 10,000 to 25,000 km2 (3,900 to 9,700 sq mi),[3] had a maximum depth of 11 metres (36 ft),[3] and a volume of 72 km3 (17 cu mi).[3]

By 2000, its extent had fallen to less than 1,500 km2 (580 sq mi). A 2001 study published in the Journal of Geophysical Research blamed the lake's retreat largely on overgrazing in the area surrounding the lake, causing desertification and a decline in vegetation.[12] The United Nations Environment Programme and the Lake Chad Basin Commission concur that at least half of the lake's decrease is attributable to shifting climate patterns. UNEP blames human water use, such as inefficient damming and irrigation methods, for the rest of the shrinkage.[13] Some consider it likely the lake will shrink further and perhaps even disappear in the course of the 21st century.

Referring to the floodplain as a lake may be misleading, as less than half of Lake Chad is covered by water through an entire year. The remaining sections are wetlands.[14] A wetland is an area of land with its soil saturated with moisture either permanently or seasonally. Such areas may also be covered partially or completely by shallow pools of water.[15] Wetlands include swamps, marshes, and bogs, among others.

Lake Chad's volume of 72 km3 (17 cu mi)[3] is very small relative to that of Lake Tanganyika (18,900 km3 (4,500 cu mi)) and Lake Victoria (2,750 km3 (660 cu mi)), African lakes with similar surface areas.

Map of the lake in 1973
Lake Chad in 1930, aerial photograph by Walter Mittelholzer


The lake is home to more than 44 species of algae, and has large areas of swamp and reedbeds. The floodplains on the southern lakeshore are covered in wetland grasses such as Echinochloa pyramidalis, Vetiveria nigritana, Oryza longistaminata, and Hyparrhenia rufa.


The entire Lake Chad basin holds 179 fish species, of which more than half are shared with the Niger River Basin, about half are shared with the Nile River Basin, and about a quarter are shared with the Congo River Basin.[16] Lake Chad itself holds 85 fish species.[16] Of the 25 endemics in the basin, only Brycinus dageti is found in the lake itself,[16] and it is perhaps better treated as a dwarf subspecies of Brycinus nurse.[17] This relatively low species richness and virtual lack of endemic fish species contrasts strongly with other large African lakes, such as Victoria, Tanganyika and Malawi.[18]

There are many floating islands in the lake. It is home to a wide variety of wildlife, including hippopotamus, crocodile (both in decline), and large communities of migrating birds including wintering ducks, ruff (Philomachus pugnax) and other waterfowl and shore birds. There are two near-endemic birds in the region, the river prinia (Prinia fluviatilis) and the rusty lark (Mirafra rufa). The shrinking of the lake is threatening nesting sites of the black-crowned crane (Balearica pavonina pavonina). During the wet season, fish move into the mineral-rich lake to breed and find food.

Threats and preservation

There is some debate over the mechanisms causing the lake's disappearance. The leading theory, which is most often cited by the UN, is that the unsustainable usage of the lake by both governments and local communities has caused the lake to be over-used, not allowing it to replenish.[19] Recently, however, an additional theory is gaining traction. This states that European air pollution had shifted rainfall patterns further south, thereby making the region dryer and not allowing the lake to replenish. Since the implementation of new regulations in the EU concerning air pollutants, much of this rainfall is now beginning to return, thereby explaining the small improvements observed since 2007.[20]

The only protected area is Lake Chad Game Reserve, which covers half of the area next to the lake that belongs to Nigeria. The whole lake has been declared a Ramsar site of international importance.

Management of the lake

The Transaqua scheme (in red) to replenish the lake.

Plans to divert the Ubangi River into Lake Chad were proposed in 1929 by Herman Sörgel in his Atlantropa project and again in the 1960s. The copious amount of water from the Ubangi would revitalize the dying Lake Chad and provide livelihood in fishing and enhanced agriculture to tens of millions of central Africans and Sahelians. Interbasin water transfer schemes were proposed in the 1980s and 1990s by Nigerian engineer J. Umolu (ZCN scheme) and Italian firm Bonifica (Transaqua scheme).[21][22][23][24][25] In 1994, the Lake Chad Basin Commission (LCBC) proposed a similar project, and at a March 2008 summit, the heads of state of the LCBC member countries committed to the diversion project.[26] In April 2008, the LCBC advertised a request for proposals for a World Bank-funded feasibility study. Neighboring countries have agreed to commit resources to restoring the lake, notably Nigeria.[27][28]

Local Impacts

Because of the way it has shrunk dramatically in recent decades, the lake has been labeled an ecological catastrophe by the UN [29] Human population expansion and unsustainable human water extraction from Lake Chad have caused several natural species to be stressed and threatened from declining lake levels. For example, the decline or disappearance of the endangered painted hunting dog has been noted in the Lake Chad area.[30]

The shrinking of the lake has also caused several different conflicts to emerge as to which countries that border Lake Chad have the rights to the remaining water. Along with the conflicts that involve the countries, violence is increasing among the lake's dwellers. Farmers and herders want the water for their crops and livestock and are constantly diverting the water.[31] The fishermen, however, want the remaining water in the lake to stay so they can continue to fish and not have to worry about the lake shrinking more and decreasing their already strained supply of fish. Furthermore, the birds and animals in the area are threatened as they are important sources of food for the local human population.

See also


  1. ^ a b Odada, Oyebande & Oguntola 2005.
  2. ^ a b WaterNews 2008.
  3. ^ a b c d e f World Lakes Database 1983.
  4. ^ United Nations 2007.
  5. ^ AllAfrica 2012.
  6. ^ Room 1994.
  7. ^ Drake & Bristow 2006, pp. 901, 910.
  8. ^ Stewart 2009.
  9. ^ Funk & Wagnalls 1973.
  10. ^ Steve Kemper (2012). Labyrinth of Kingdoms: 10,000 Miles Through Islamic Africa. W. W. Norton.  
  11. ^ Drake & Bristow 2006, Figures 1, 10.
  12. ^ Coe & Foley 2001.
  13. ^ CNN 2007.
  14. ^ Braun 2010.
  15. ^ PBS 2009.
  16. ^ a b c Hughes & Hughes 1992.
  17. ^ Froese, Rainer and Pauly, Daniel, eds. (2011). "Brycinus nurse in FishBase. May 2011 version.
  18. ^ Nelson 2006.
  19. ^
  20. ^
  21. ^ Bunu 1999.
  22. ^ Pearce 1991.
  23. ^ Umolu 1990, pp. 218-262.
  24. ^ Chapman & Baker 1992.
  25. ^ Umolu 1994, Section X.
  26. ^ Voice of America 2008.
  27. ^
  28. ^
  29. ^ Voice of America 2009.
  30. ^ Hogan 2009.
  31. ^


External links

  • Bibliography on Water Resources and International Law Peace Palace Library
  • International Cooperation and Sustainable Water Management of the Waters of the Lake Chad/ by Moustapha Abakar Malloumi
  • The Encyclopedia of Earth: Lake Chad flooded savanna
  • Information on, and a map of, Chad's watershed.
  • Map of the Lake Chad basin at Water Resources eAtlas.
  • Article on the disappearing lake in The Guardian.
  • Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data.

This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from World Library are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.