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・ Tana FC Formation
・ Tana French
・ Tana Glacier
・ Tana Goertz
・ Tana Hoban
・ Tana labeo
・ Tana language
・ Tana Louise
・ Tana Mana
・ Tana Moon
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・ Tana River (Cuba)
Tana River (Kenya)
・ Tana River cisticola
・ Tana River County
・ Tana River Delta Ramsar Site
・ Tana River mangabey
・ Tana River Primate National Reserve
・ Tana River red colobus
・ Tana Senn
・ Tana Sripandorn
・ Tana Station
・ Tana Tani
・ Tana Tidung Regency
・ Tana Toa
・ Tana Toraja Regency
・ Tana Umaga


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Tana River (Kenya) : ウィキペディア英語版
Tana River (Kenya)

The long Tana River is the longest river in Kenya, and gives its name to the Tana River County.〔Nakaegawa T., Wachana C. and KAKUSHIN Team-3 Modeling Group. (2012). "First impact assessment of hydrological cycle in the Tana River Basin, Kenya, under a changing climate in the late 21st Century," (''Hydrological Research Letters'', 6, pp. 29-34 ).〕 Its tributaries include the Thika, as well as several smaller rivers that flow only during the rainy season. The river rises in the Aberdare Mountains to the west of Nyeri. Initially it runs east before turning south around the massif of Mount Kenya. The river then runs into the Masinga Reservoir and Kiambere Reservoir, created by the Kindaruma dam. Below the dam the river turns north and flows along the north-south boundary between the Meru and North Kitui and Bisanadi, Kora and Rabole National Reserves. In the reserves the river turns east, and then south east. It passes through the towns of Garissa, Hola and Garsen before entering the Indian Ocean at Ungwana Bay-Kipini area, at the end of a river delta that reaches roughly 30 km upstream from the river mouth itself.〔
Annual flow is above 5,000 million cubic meters (MCM) on average, but varies substantially both within and across years, and includes two flood seasons each year. Between 1944 and 1978, average total flow (at Garissa) was 6,105 MCM, varying from only 1,789 MCM in 1949 to 13,342 MCM in 1968.〔Hughes, F. (1990). "The Influence of Flooding Regimes on Forest Distribution and Composition in the Tana River Floodplain, Kenya," (''Journal of Applied Ecology'', 27(2), pp. 475-491 ).〕 During the 1982-1996 period, annual flow remained above 5,000 MCM as well.〔Maingi, J.K. and Marsh, S.E. (2002). "Quantifying hydrologic impacts following dam construction along the Tana River, Kenya," (''Journal of Arid Environments'', 50, pp. 53-79 ).〕 A series of hydroelectric dams have been constructed along the river, including the Kindaruma Dam in 1968, the Kamburu Dam in 1975, the Gitaru Dam in 1978, the Masinga Dam in 1981, and the Kiambere Dam in 1988.〔Adams, W. M. and Hughes, F. M. R. (1986). "The Environmental Effects of Dam Construction in Tropical Africa: Impacts and Planning Procedures," (''Geoforum'', 17(3), pp. 403-410 ).〕 A 2003 study reported that two-thirds of Kenya's electrical needs were supplied by the series of dams along the Tana River.
== See also ==

* Tana River Primate Reserve

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