Jump to content

Lake Chad

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Newbamboo (talk | contribs) at 13:43, 24 March 2024. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

This article is about the lake in Africa. For the lake in Antarctica, see Lake Chad (Antarctica).

Lake Chad
LocationSahelian zone at the conjunction of Chad, Cameroon, Nigeria, and Niger
Primary inflowsChari River, Yobe River, Ngadda River
Primary outflowsBahr el-Ghazal
Basin countriesChad, Cameroon, Nigeria, Niger
Surface area2,000 km2 (770 sq mi)
Max. depth2 m (6.6 ft)
IslandsBogomerom Archipelago
Settlements
Official nameLac Tchad
Designated17 June 2001
Reference no.1072[1]
Official namePartie tchadienne du lac Tchad
Designated14 August 2001
Reference no.1134[2]
Official nameLake Chad Wetlands in Nigeria
Designated30 April 2008
Reference no.1749[3]
Official namePartie Camerounaise du Lac Tchad
Designated2 February 2010
Reference no.1903[4]

Lake Chad (Template:Lang-ar, Kanuri: Sádǝ, Template:Lang-fr) is an endorheic freshwater lake located at the junction of four countries: Nigeria, Niger, Chad, and Cameroon in western and central Africa respectively, with a catchment area of 1 million square kilometres (390,000 sq mi). Lake Chad is divided into deeper southern parts and shallower northern parts. The water source of the lake mainly comes from rivers such as the Chari River that enter the lake. The water level varies greatly seasonally, and the area of the lake also changes dramatically.

During the African humid period, The area of Lake Chad reached 400,000 square kilometres (150,000 sq mi). Due to the increasingly arid climate, the lake surface gradually shrank. In the 19th century, Lake Chad still had an area of 28,000 square kilometres (11,000 sq mi). However, due to climate change and human water diversion, Lake Chad has been greatly reduced since the mid-1970s, and its area has fluctuated between 2,000 and 5,000 square kilometres (770 and 1,930 sq mi).

Lake Chad is also an important wetland ecosystem in West-Central Africa. The lakeside is rich in reeds and swamps, and the plain along the lake is fertile, making it an important irrigated agricultural area. The lake is rich in aquatic resources and is one of the important freshwater fish producing areas in Africa.

History

Lake Chad in African humid period (blue) and in 20th century (green)

The Chad Basin was formed by the depression of the African Shield.[5][6][7] For most of the Quaternary, the basin had abundant water sources. Towards the end of this period the climate became drier. Around 20,000-40,000 years ago, eolianite sand dunes began to form in the north of the basin.[8] The area of Lake Chad experienced four heydays between 39,000 BC and 300 BC, leaving thick diatomaceous earth and lacustrine deposits in the strata. This has been called Mega-Chad. The maximum depth of Mega-Chad exceeds 180 metres (590 ft) and covers an area of approximately 400,000 square kilometres (150,000 sq mi),[5] flowed into the Benue River through the Mayo Kébbi, and finally flows into the Atlantic Ocean through the Niger River.[9]

The vast waters formed during the African humid period provided conditions for the emergence of lakeside fishermen's settlements, and the Nilo-Saharan ethnic group also migrated to Lake Chad during this period. Agriculture also emerged in the Sahel region at this time.[10] The archaeological discovery revealed Paniceae and wild rice together with the earliest domesticated Pearl millet in the Lake Chad region, dating to 1200-1000 cal BC. One of the oldest domesticated Pearl millet in West Africa was found in Lake Chad baisn, charred together with wild grasses, mostly of the tribe Paniceae, and their era can be traced back to 800-1000 cal BC.[11]

In the 5th century BC, the Sao civilization emerged in the Lake Chad region.[5] According to the records of Claudius Ptolemy in the mid-2nd century AD, the Romans of the 1st century AD had already come into contact with Lake Chad through their connections with Tunisia, Tripolitania, and Fezzan. But later on, even Arabs and Moors familiar with the geography of the Sudan region often confused Lake Chad with the Niger river or Nile river systems.[12]

Around 900 AD, the Kanem people who spoke the Kanuri language unified numerous nomadic tribes and established the Kanem Empire in the northeast of Lake Chad. At the beginning of the founding of the country, the Kanem people continued to live a nomadic life until the 11th century, when they were Islamized and settled in Njimi. Through trans-Saharan trade, the power of the Kanem Empire reached its peak in the 13th century, but as the empire declined in the 14th century, its southwestern vassal state of Bornu began to rise, causing the power center of the empire to shift to Bornu around 1400. In the second half of the 16th century, Bornu Empire began importing firearms from North Africa, consolidating its military hegemony. Bornu Empire declined in the 18th century, and the rebellion of the Fulani herders caused Bornu to lose its western region and be conquered by France in the late 19th century.[13]

Following the growing interest in Africa among European academic and business communities, the Lake Chad area was extensively described by Europeans in the 19th century.[5] Gustav Nachtigal of Prussia carried a gift from the King of Prussia and established connections with the rulers of the Bornu Empire on the shores of Lake Chad; Hanns Vischer of Switzerland crossed the Sahara Desert with a camera and arrived at Lake Chad, taking a large number of photos; Boyd Alexander of Britain completed an exploration journey from the Atlantic to the Red Sea in order to explore the relationship between the Niger River, Lake Chad, and the Nile River. By the second decade of the 20th century, Lake Chad had been colonized and occupied by Britain, France, and Germany.[14]

Geography

Map showing the Chari River drainage basin

The Lake Chad Basin is an extensional fault depression type rift basin, which can be divided into four secondary structural units: southern depression, northern depression, central uplift, and eastern slope. The southern depression of the basin is characterized by an asymmetric fault depression composite rift with steep slopes in the east and gentle slopes in the west on the profile, and is distributed in an NNW direction on the plane. There are two large basin‐bounding normal fault developed on both sides of the basin, with a graben style fault and depression in the middle. The east and west sides are outward dipping low angle gentle slope areas. The eastern boundary fault is steep with a dip angle of about 55 °, while the western fault has a dip angle of about 45 °. The overall thickness of the inner layer in the slope area is relatively thin. In the central area of the basin, the thickness of the sedimentary strata is large, and the thickness of the sedimentary center zone reaches over 10,000 metres (33,000 ft). The northern part of the basin appears steep in the west and gentle in the east on the profile. Five fault structural zones parallel to the basin‐bounding faults have developed from west to east.[15]

Lake Chad is divided into north and south parts by a shallow sill called the Great Barrier, with the bottom of the northern basin at an altitude of 275.3 metres (903 ft) and the bottom of the southern basin at 278.2 metres (913 ft). When the water level in the south exceeds 279 metres (915 ft) above sea level, it will flow into the north.[16] In the south, there is continuous open water at the mouth of the Chari River, and the western part of the water is covered by reed swamps,[17] and the sand dunes that are not completely submerged in the eastern waters form an archipelago.[7] The average depth of the southern lake basin is between .5 and 2 metres (1.6 and 6.6 ft), that of the northern lake basin is between 0 and 1.8 metres (5.9 ft), and that of the eastern archipelago is between 0 and 2 metres (6.6 ft).[18]

The climate of the Lake Chad region is strongly influenced by continental and maritime air masses. The maritime air mass moves northward during the summer, producing seasonal precipitation. In late summer, continental air mass dominate again.[5] The average annual precipitation in the Lake Chad area is 330 mm, with an average annual precipitation of 560 mm on the south bank and about 250 mm on the north bank. The highest temperature in the rainy season is 30 °C, and the highest temperature rises to more than 32 °C when October and November enter the dry season. The temperature difference between day and night is almost twice that of the rainy season, and the lowest nighttime temperature sometimes drops to 8 °C in December and January. April is usually the hottest month of the year, with temperatures occasionally reaching 40 °C, the lowest water levels appear in June to July, and the highest water levels in November to December, with surface water temperatures ranging from 19 °C to 32 °C.[5][7]

Hydrology

Lake Chad 1972–2007

The Lake Chad basin covers an area of about 1 million square kilometres (390,000 sq mi), and is injected by the Shari River, Engada River, and Yobe River.[7][5] The water supply of the lake is seasonal. Most of the precipitation comes from the Adamawa Plateau in the south of the basin, which is transported to the lake basin through the Chari River and the Logone River. The two contribute 95% of the total inflow of Lake Chad, while the Yobe River only contributes less than 2.5%. The lake seeps through the underground to the lowest point of the Chad Basin,[19] the Bodélé Depression, approximately 480 kilometres (300 mi) northeast of Lake Chad, with the deepest point reaching an elevation of only 155 metres (509 ft) above sea level. [20] This takes away most of the salinity and maintains the low salinity of Lake Chad. The southwestern waters of Lake Chad being freshwater, and the water in the northeast is only slightly salty.[19][6]

The water volume of most large lakes in Africa depends on rainfall and evaporation, which means that temperature and precipitation are crucial for regulating the water balance of these bodies of water, and any fluctuations can cause significant changes in their water level and area.[21] Lake Chad is a shallow inland lake, and the rainfall in the Lake Chad basin is very sensitive to small changes in atmospheric circulation, so the surface area of Lake Chad is greatly affected by climate change.[22][23] Dry climate due to vegetation loss from overgrazing and deforestation and large-scale irrigation projects that diverted water from the rivers that feed the lake are the main reasons for the shrinkage of Lake Chad.[24] the Atlantic multidecadal oscillation and the El Niño–Southern Oscillation have affected precipitation in the Sahel region. From the early 1960s to the mid-1980s, the lake water level decreased by 3 metres (9.8 ft) compared to the average level from 1900 to 2010.[25]

In 1870, the area of Lake Chad was about 28,000 square kilometres (11,000 sq mi). The lake was able to flow out of the Bahr el-Ghazal during the rainy season. At the turn of the 20th century the area of Lake Chad shrank briefly, and reached a new high in the middle of the 20th century and overflowed from the Bahr el-Ghazal again.[5] A major drought started in the Sahel region in the late 1960s and caused severe damage in 1972 and 1984. It was thought to be related to vegetation loss, global warming, and sea surface temperature anomalies.[22] During this period, Lake Chad shrunk considerably and fluctuated in the range of 2,000 to 5,000 square kilometres (770 to 1,930 sq mi) thereafter.[16]

From June 1966 to January 1973, the area of Lake Chad shrank from 22,772 square kilometres (8,792 sq mi) to 15,400 square kilometres (5,900 sq mi),[24] further shrunk to 4,398 square kilometres (1,698 sq mi) in 1975,[16] and only 1,756 square kilometres (678 sq mi) in February 1994.[24] Since then, the area of Lake Chad has entered a relatively stable stage with a slight increase.[26] From 1995 to 1998, it fluctuated within the range of 1,200 to 4,500 square kilometres (460 to 1,740 sq mi). The area once reached 5,075 square kilometres (1,959 sq mi) in 2000,[16] and the average area of surface water from 2013 to 2016 was about 1,876 square kilometres (724 sq mi), with the largest area being 2,231 square kilometres (861 sq mi) in July 2015.[27]

Ecology

Lake Chad flooded savanna

Part of the Lake Chad Basin is located within the Chad Basin National Park in Nigeria, and the country and Cameroon have established the Lake Chad Ramsar Wetland with a total area of 8,225 km2.[28] The wetland plants in the south mainly include cyperus papyrus, etc. Reeds mainly grow in the north where the salinity is high, and the floating plant pistia sometimes covers large areas of open water. Plants such as hyparrhenia rufa grow on the shores of lakes with long floods in the south.[28] The area of permanent vegetation has increased from about 3,800 square kilometres (1,500 sq mi) in 2000 to about 5,200 square kilometres (2,000 sq mi) in 2020 as water levels have dropped and temperatures have increased.[29] The surrounding dense woodland has been converted to open forest with acacias, baobabs, palms and Indian jujube.[5]

Lake Chad is permanently or seasonally inhabited by hundreds of species of birds such as northern shoveler, Egyptian goose and marabou stork.[5] It is an important wintering ground for European anatididae and wading birds. There are raptors such as steppe eagle and booted eagle on the lakeshore,[28] and more than one million ruff can be observed on the lake at one time.[30] The once common large mammals include red-fronted gazelle, dama gazelle, patas monkey, striped hyena, cheetah and caracal, while African elephant, otter, hippopotamus, sitatunga and kob are distributed in the wetlands. At present, most of the large mammals have been hunted to extinction, replaced by a large number of cattle.[28]

The entire Lake Chad Basin has 179 species of fish, of which 127 are the same as the Niger River Basin, 85 are the same as the Nile River Basin, 47 are the same as the Congo River Basin, and 84 fish species are distributed in the lake.[6] This makes it a rich fishing ground for communities across Nigeria, Niger, Chad, and Cameroon. The seasonal influx of floods combined with seasonal increases in air temperature leads to decreased salinity, increased turbidity, and increased trophic levels, which catalyzed a surge in the number of phytoplankton and zooplankton, allowing large fish to migrate seasonally within the watershed to feed and breed in the fertile floodplain when floods arrive.[17]

Development

Lake Chad replenishment project
Lake Chad in a 2001 satellite image, with the actual lake in blue. The lake lost more than 90% of its surface area between 1987 and 2005.[31]

Local self-sufficient crops include sorghum, maize, finger millet, beans, and vegetables. Gourd is widely planted for making utensils. The collection of forest products such as gum arabic, honey, beeswax, and firewood is of great significance in the region. However, the reduction in forest area has had a negative impact on the production of these products, and the explosive growth of cattle herds has exacerbated this impact. Cattle are the most important livestock raised, as well as poultry, goats, sheep, camels, horses, and donkeys. The livestock industry was severely affected by the droughts of the 1970s and 1980s. Fishing has traditionally been the most important economic activity for the people of the lake area, which almost ceased during drought periods and only resumed in the mid-1990s. Most fishing products are dried, pickled, or smoked. The natron produced in the depression on the northeast bank of the lake has long been of significant economic significance. Traditionally, it has been excavated in blocks and transported across the lake to enter the Nigerian market.[5]

There are more than 30 million residents in the Chad Lake Basin. There are more than 70 ethnic groups around the lake, most of whom are distributed on the south bank, where the population density exceeds 100 inhabitants per square kilometre (260/sq mi). They rely on the water source of Chad Lake for irrigation, breeding, animal husbandry and drinking.[19] Since the drought in the 1970s, the soil that can be planted without irrigation and fertilization has been exposed at the bottom of the lake, and it has been reclaimed as a polder for planting maize, cowpea, rice, sorghum and other crops.[32] Farmers have shifted from planting mainly dry crops, such as wheat, to rice with high water demand, resulting in more serious soil salinization and water eutrophication.[19]

Since 1970, five countries in the southern part of the basin have constructed numerous water conservancy projects in the upper reaches of the Chari River, Logone River, and Yobe River to intercept river water, resulting in a sharp decrease in the amount of water entering the lake. The average annual inflow of the Chari River and the Logone River from 1970 to 1990 was only 55% of that from 1950 to 1970. Since the 1980s, one-third of the water in the Chari River and the Logone River has been diverted and intercepted by the Central African Republic located upstream for agricultural irrigation and hydroelectric power generation.[19] The dams built on the upper reaches of the rivers entering the lake changed the time and scope of seasonal floods and disrupted the migration of fish, resulting in a sharp reduction in the populations of Alestes baremoze and Nile perch, the main catches of Lake Chad, and a significant reduction in the catch.[30][6] At the same time, the conflicts between countries and ethnic groups competing for water and land are also escalating. The four countries along the lake are all facing the problem of extreme poverty, and due to the difficulty in meeting their livelihoods, some local residents have been involved in drug and arms trade, and even spawned terrorist organizations such as Boko Haram.[19]

Cameroon, Niger, Nigeria, and Chad established the Lake Chad Basin Commission on 22 May 1964. The Central African Republic joined in 1996, and Libya joined in 2008. The headquarters of the committee is located in N'Djamena, Chad. The commission's tasks include managing Lake Chad and its water resources, protecting the ecosystem, and promoting regional integration, peace, security, and development in the Lake Chad region.[33] The surrounding countries' water replenishment plan for Lake Chad includes the construction of a 2,400 kilometres (1,500 mi) canal to transport 100 billion cubic metres (130×10^9 cu yd) of water from the Congo River Basin to the Chari River Basin every year, and use a series of dams along the route to generate electricity.[34]

See also

References

  1. ^ "Lac Tchad". Ramsar Sites Information Service. Archived from the original on 23 June 2018. Retrieved 25 April 2018.
  2. ^ "Partie tchadienne du lac Tchad". Ramsar Sites Information Service. Archived from the original on 23 June 2018. Retrieved 25 April 2018.
  3. ^ "Lake Chad Wetlands in Nigeria". Ramsar Sites Information Service. Archived from the original on 23 June 2018. Retrieved 25 April 2018.
  4. ^ "Partie Camerounaise du Lac Tchad". Ramsar Sites Information Service. Archived from the original on 1 February 2020. Retrieved 25 April 2018.
  5. ^ a b c d e f g h i j k Gritzner, J. A. "Lake Chad". Encyclopedia Britannica. Chicago: Encyclopædia Britannica, Inc. Archived from the original on 22 July 2019. Retrieved 13 June 2023.
  6. ^ a b c d Hughes, R. H.; Hughes, J. S. (1992). A Directory of African Wetlands (PDF). IUCN / UNEP / WCMC. pp. 329–330. ISBN 2-88032-949-3. Archived (PDF) from the original on 24 September 2012. Retrieved 14 June 2023.
  7. ^ a b c d Wen Yunzhao. "Lake Chad". Encyclopedia of China (in Chinese (China)) (03 ed.). Beijing: Encyclopedia of China Publishing House. Archived from the original on 13 June 2023. Retrieved 11 June 2023.
  8. ^ Wright, J.B. (30 November 1985). Geology and Mineral Resources of West Africa. Springer. p. 95. ISBN 978-0-04-556001-1. Retrieved 6 May 2013.
  9. ^ Leblanc, M.; Favreau, G.; Maley, J.; Nazoumou, Y.; Leduc, C.; Stagnitti, F.; van Oevelen, P. J.; Delclaux, F.; Lemoalle, J. (2006). "Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data". Palaeogeography, Palaeoclimatology, Palaeoecology. 239 (1–2): 16–27. doi:10.1016/j.palaeo.2006.01.003. Archived from the original on 13 June 2023. Retrieved 13 June 2023.
  10. ^ Shillington, Kevin. 非洲通史 (in Chinese) (4 ed.). 九州出版社. pp. 13+19. ISBN 978-7-5108-9793-1.
  11. ^ Marlies Klee; Barbara Zach (1999). "The Exploitation of Wild and Domesticated Food Plants at Settlement Mounds in North-East Nigeria (1800 cal BC to Today)". The Exploitation of Plant Resources in Ancient Africa: 81–88. doi:10.1007/978-1-4757-6730-8_8.
  12. ^ Johnston, H. H. (1910). "Lake Chad". Nature. 84 (2130): 244–245. Bibcode:1910Natur..84..244J. doi:10.1038/084244a0. ISSN 1476-4687. S2CID 8682184.
  13. ^ Shillington, Kevin. 非洲通史 (in Chinese) (4 ed.). 九州出版社. pp. 97-98+188-190+254-255. ISBN 978-7-5108-9793-1.
  14. ^ 熊正坤; 张瑾 (8 April 2021). "乍得湖：从"文明摇篮"到"死亡之心"" [Lake Chad: From "Cradle of Civilization" to "Heart of Death"]. China Water Resources News. Archived from the original on 1 January 2024. Retrieved 1 January 2024.
  15. ^ 黄先雄; 夏斌; 万志峰; 吕宝凤; 蔡周荣 (2008). "乍得湖盆地构造特征与油气成藏规律初探" [A preliminary study on the tectonic characteristics and hydrocarbon accumulation law of the Lake Chad Basin]. 大地构造与成矿学 (03): 326–331. doi:10.16539/j.ddgzyckx.2008.03.013.
  16. ^ a b c d 刘甜甜; 刘荣高; 葛全胜 (2013). "基于多源遥感数据的非洲乍得湖水面变化监测" [Monitoring of water surface change in Lake Chad in Africa based on multi-source remote sensing data]. 地理科学进展 (in Chinese (China)). 32 (6): 906–912. doi:10.11820/dlkxjz.2013.06.007.
  17. ^ a b Marie-Thérèse Sarch; Charon Birkett (June 2000). "Fishing and farming at Lake Chad: Responses to lake-level fluctuations". The Geographical Journal. 166 (2): 156–172. JSTOR 823109. Archived from the original on 18 June 2023. Retrieved 18 June 2023.
  18. ^ Jacques Lemoalle; Jean-Claude Bader; Marc Leblanc; Ahmed Sedick (January 2012). "Recent changes in Lake Chad: Observations, simulations and management options (1973–2011)". Global and Planetary Change. 80–81 (247–254): 247–254. doi:10.1016/j.gloplacha.2011.07.004.
  19. ^ a b c d e f 袁宣民 (2016). "乍得湖的环境、安全及其脆弱性" [The environment, security and vulnerability of Lake Chad]. 世界科学 (in Chinese (China)) (7): 21–23. Archived from the original on 21 March 2023. Retrieved 13 June 2023.
  20. ^ "Geography". Lake Chad Basin Commission. Archived from the original on 6 January 2019. Retrieved 5 May 2013.
  21. ^ Richard Ogutu-Ohwayo; Vianny Natugonza; Laban Musinguzi; Mark Olokotum; Shamim Naigaga (2016). "Implications of climate variability and change for African lake ecosystems, fisheries productivity, and livelihoods". Journal of Great Lakes Research. 42 (03): 498–510. doi:10.1016/j.jglr.2016.03.004.
  22. ^ a b Evans, T. (1996). "The effects of changes in the world hydrological cycle on availability of water resources". In Bazzaz, F.; Sombroek, W. (eds.). Global climate change and agricultural production. FAO / John Wiley & Sons. ISBN 92-5-103987-9. Archived from the original on 18 June 2023.
  23. ^ Leblanc, M.; Favreau, G.; Tweed, S. (2007). "Remote sensing for groundwater modelling in large semiarid areas:Lake Chad Basin, Africa". Hydrogeology Journal. 15: 97–100. doi:10.1007/s10040-006-0126-0.
  24. ^ a b c "Lake Chad: almost gone". United Nations Environment Programme (UNEP). Archived from the original on 16 December 2008. Retrieved 5 December 2015.
  25. ^ Churchill Okonkwo; Belay Demoz; Ricardo Sakai; Charles Ichoku; Chigozie Anarado; Jimmy Adegoke; Angelina Amadou; Sanusi Imran Abdullahi; Nir Krakauer (15 December 2015). "Combined effect of El Niño southern oscillation and Atlantic multidecadal oscillation on Lake Chad level variability". Cogent Geoscience. 1 (1). doi:10.1080/23312041.2015.1117829. Archived from the original on 24 December 2023. Retrieved 24 December 2023.
  26. ^ Wengbin Zhu; Jiabao Yan; Shaofeng Jia (2017). "Monitoring Recent Fluctuations of the Southern Pool of Lake Chad Using Multiple Remote Sensing Data: Implications for Water Balance Analysis". Remote Sensing. 9 (10): 1032. doi:10.3390/rs9101032.
  27. ^ Willibroad Gabila Buma; Sang-Il Lee; Jae Young Seo (2018). "Recent surface water extent of Lake Chad from multispectral sensors and GRACE". Sensors. 18 (7): 2082. doi:10.3390/s18072082. PMC 6069056. PMID 29958481.
  28. ^ a b c d Emma Martin; Neil Burgess. "Lake Chad Flooded Savanna". www.oneearth.org. Archived from the original on 15 July 2023. Retrieved 15 July 2023.
  29. ^ Binh Pham-Duc; Florence Sylvestre; Fabrice Papa; Frédéric Frappart; Camille Bouchez; Jean-Francois Crétaux (2020). "The Lake Chad hydrology under current climate change". Scientific Reports. 10 (5498). doi:10.1038/s41598-020-62417-w. PMC 7099084.
  30. ^ a b Keith, J. O.; Plowes, D. C. H. (March 1997). Considerations of Wildlife Resources and Land Use in Chad (PDF) (Report). Office of Sustainable Development, Africa Bureau, USAID. p. 3. SD Technical Paper No. 45. Archived from the original (PDF) on 18 June 2023.
  31. ^ Onamuti, Olapeju Y.; Okogbue, Emmanuel C.; Orimoloye, Israel R. (8 November 2017). "Remote sensing appraisal of Lake Chad shrinkage connotes severe impacts on green economics and socio-economics of the catchment area". Royal Society Open Science. 4 (11): 171120. doi:10.1098/rsos.171120. PMC 5717671. PMID 29291097.
  32. ^ Luxereau, A.; Genthon, P.; Ambouta, J.-M. K. (2011). "Fluctuations in the Size of Lake Chad: Consequences on the Livelihoods of the Riverain Peoples in Eastern Niger". Regional Environmental Change. 12 (3): 507–521. doi:10.1007/s10113-011-0267-0. Archived from the original on 14 June 2023. Retrieved 13 June 2023.
  33. ^ "About us". Lake Chad Basin Commission. Archived from the original on 15 July 2023. Retrieved 15 July 2023.
  34. ^ Ross, Will (31 March 2018). "Can the vanishing lake be saved?". BBC. Archived from the original on 9 August 2019. Retrieved 28 January 2019.

Further reading

  • Hughes, R. H.; Hughes, J. S. (1992). A Directory of African Wetlands. IUCN. ISBN 978-2-88032-949-5.
  • Beadle, L. C. (1974). The Inland Waters of Tropical Africa: An Introduction to Tropical Limnology Hardcover (1th ed.). Longman Publishing Group. ISBN 978-0582448520.
  • Chapman, Graham; Baker, Kathleen M. (1992). The changing geography of Africa and the Middle East. Routledge. ISBN 9780203034507.
  • Caterina Batello; Marzio Marzot; Adamou Harouna Touré (2004). The Future is an Ancient Lake. FAO Interdepartmental Working Group on Biological Diversity for Food and Agriculture. ISBN 92-5-105064-3.
Wikimedia Commons has media related to:
Lake Chad (category)
Retrieved from "https://en.wikipedia.org/enwiki/w/index.php?title=Lake_Chad&oldid=1215331113"