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Contents

   



(Top)
 


1 Climate  





2 See also  





3 Notes  





4 External links  














Lake Abaya







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Coordinates: 6°26N 37°53E / 6.433°N 37.883°E / 6.433; 37.883
 

From Wikipedia, the free encyclopedia
 


Lake Abaya
Location of Lake Abaya in Ethiopia.
Location of Lake Abaya in Ethiopia.

Lake Abaya

Coordinates6°26′N 37°53′E / 6.433°N 37.883°E / 6.433; 37.883
Primary inflowsBilate River
Gidabo River
Gelana River
Basin countriesEthiopia
Max. length60 km (37 mi)
Max. width20 km (12 mi)
Surface area1,162 km2 (449 sq mi)
Average depth7.1 m (23 ft)
Max. depth13.1 m (43 ft)
Water volume8.2 km3 (2.0 cu mi)
Surface elevation1,175 m (3,855 ft)
SettlementsArba Minch
Lake Abaya as seen from a Dorze village. On the far right Arba Minch and Lake Chamo can be seen. Between the two lakes is the Nechisar National Park.

Lake Abaya (Amharic: አባያ ሐይቅ) is a lake in the Southern Nations, Nationalities, and Peoples' RegionofEthiopia. It is located in the Main Ethiopian Rift, east of the Guge Mountains.

The town of Arba Minch lies on its southwestern shore, and the southern shores are part of the Nechisar National Park. Just to the south is Lake Chamo. Savanna, known for its wildlife and birdlife, surrounds the lake, which is also fished by local people. According to the Ethiopian Department of Fisheries and Aquaculture, 412 tonnes of fish are landed each year, which the department estimates is 69% of its sustainable amount.[1]

Lake Abaya is 60 kilometers long and 20 wide,[2] with a surface area of 1162 square kilometers.[3] There are a number of islands in this lake, the largest being Aruro;[4] others include Gidicho, Welege, Galmaka, and Alkali. The lake is red due to a high load of suspended sediments.[5]

The lake is fed by three medium-sized rivers. First there is the Bilate which rises on the southern slopes of Mount Gurage, then runs mostly southward to drain into Lake Abaya at its northern shore. Second, there is the Gidabo, which rises on the western slopes of the Bale Mountains, then also runs mostly southwards to drain into Lake Abaya at its northeastern tip after having passed the Gidabo flood plains. A third river is the Gelana, which rises at the western escarpment of the Rift Valley northwest of Bule Hora Town. Tributary streams also rise on the eastern and northern slopes of the Amaro Mountains. The Gelana then flows northwards through the Gelana Graben in the middle between both mountain ranges before it enters the Bore swamps and finally drains on the eastern side into the lake.

The only outflow of the lake is through the lower reaches of Kulfo River directly below an alluvial fan at an elevation of 1,190 m (at6°00′39N 37°35′07E / 6.0109°N 37.5854°E / 6.0109; 37.5854). The riverbed acts as an spillway in the case of high lake levels and discharges the excess water into Lake Chamo. Usually, the lake level oscillates somewhat, in 2017 it was at 1,175 m, 15 m below the overflow level.[6] In the last 50 years, the lake level oscillated only ±1.5 m around a mean value which is well below the overflow level.[7] Consequently, the maximum depth of the lake changes only slightly from year to year, in the year 2002 the lake had a maximum depth of 13.1 meters.[3]

In 1896 Lake Abaya was renamed "Lake Margherita" after the Queen Margherita of Savoy, wife of King Humbert I of Italy by the Italian explorer Vittorio Bottego who first explored the region. The name "Lake Margherita" (Lago Margherita) is still used in Italy.[8]

Climate[edit]

Climate data for Lake Abaya (Bilate), elevation 1,200 m (3,900 ft), (1971–2000)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 31.9
(89.4)
32.0
(89.6)
32.4
(90.3)
29.0
(84.2)
29.6
(85.3)
28.1
(82.6)
26.3
(79.3)
26.4
(79.5)
28.5
(83.3)
29.2
(84.6)
30.4
(86.7)
30.5
(86.9)
29.5
(85.1)
Mean daily minimum °C (°F) 15.3
(59.5)
14.9
(58.8)
15.2
(59.4)
16.1
(61.0)
16.2
(61.2)
16.1
(61.0)
16.0
(60.8)
16.0
(60.8)
15.4
(59.7)
14.1
(57.4)
15.0
(59.0)
14.5
(58.1)
15.4
(59.7)
Average precipitation mm (inches) 20.0
(0.79)
22.0
(0.87)
74.0
(2.91)
91.0
(3.58)
98.0
(3.86)
89.0
(3.50)
104.0
(4.09)
91.0
(3.58)
73.0
(2.87)
41.0
(1.61)
17.0
(0.67)
14.0
(0.55)
734
(28.88)
Average relative humidity (%) 57 54 59 63 74 75 78 77 77 71 58 53 66
Source: FAO[9]

See also[edit]

Notes[edit]

  • ^ Statistical Abstract of Ethiopia for 1967/68
  • ^ a b Baxter, R. M. Lake Morphology and Chemistry. in Taylor, W.D. and Tudorancea, C., eds. Ethiopian Rift Valley Lakes. Leiden: Backhuys Publishers, 2002.
  • ^ "Local History in Ethiopia" Archived 2007-09-27 at the Wayback Machine The Nordic Africa Institute website (accessed 5 November 2007)
  • ^ A. T. Grove; F. A. Street; A. S. Goudie, 1975: "Former Lake Levels and Climatic Change in the Rift Valley of Southern Ethiopia," Geographical Journal 141, 177-194
  • ^ Google Earth
  • ^ Ababu Teklemariam, Bernd Wenclawia (2004). "Water Quality monitoring within the Abaya-Chamo Drainage Basin" (PDF). Archived from the original (PDF) on 2018-02-07. Retrieved 2018-02-06.
  • ^ Mack Smith, Denis. Mussolini’s Roman Empire. New York: Viking, 1976.
  • ^ "CLIMWAT climatic database". Food and Agriculture Organization of United Nations. Retrieved 23 June 2024.
  • External links[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Lake_Abaya&oldid=1230553940"

    Categories: 
    Lakes of Ethiopia
    Lakes of the Great Rift Valley
    Southern Nations, Nationalities, and Peoples' Region
    Endorheic lakes of Africa
    Hidden categories: 
    Pages using gadget WikiMiniAtlas
    Webarchive template wayback links
    Coordinates on Wikidata
    Articles using infobox body of water without alt
    Articles using infobox body of water without alt bathymetry
    Articles with VIAF identifiers
     



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