South Aral Sea
|South Aral Sea|
The Aral Sea in 2011. The three lakes to the south and west are the remains of the South Aral Sea.
|Type||endorheic, natural lake|
|Primary inflows||groundwater only
(previously the Amu Darya)
|Basin countries||Kazakhstan, Uzbekistan|
|Surface area||West Aral Sea:
3,500 km2 (1,350 sq mi) (2005)
(fluctuating area of Eastern Sea)
42,100 km2 (16,250 sq mi) (1989)
|Average depth||14–15 m (46–49 ft) (2005)|
|Max. depth||37–40 m (121–131 ft) (2005)|
|Surface elevation||29 m (95 ft) (2007)|
The South Aral Sea was a lake in the basin of the former Aral Sea which formed in 1986 when that body divided in two, due to diversion of river inflow for agriculture. In 2003 the South Aral Sea itself split into eastern and western basins, the Eastern Sea (now the Aralkum) and the West Aral Sea, connected by a narrow channel (channel bed at an elevation of 29 m (95 ft)) that balanced surface levels but did not allow mixing, and in 2005 the North Aral Sea was dammed to prevent the collapse of its fisheries, cutting off the only remaining inflow to the southern lakes. In 2008 the Eastern Sea split again, and in May 2009 had completely dried out. In 2010, it was partially filled again by meltwater. The West Aral Sea has some replenishment from groundwater in the northwest, and so is likely to avoid desiccation.
The Aral Sea began shrinking in the 1960s, when the Soviet Union decided that the two rivers feeding it, the Amu Darya and the Syr Darya, would be diverted to irrigate cotton and food crops in Kazakhstan and Uzbekistan. In 1986, due to an accelerated loss of water, the Aral Sea was split into northern and southern parts; the northern part is the current North Aral Sea.
In 2007, the western basin had a salinity of 70 g/l and the eastern basin 100 g/l. Once the water level falls below the connecting channel (elevation 29 m), the salinities can be expected to diverge further. Under current conditions, the eastern basin may receive water from the Amu Darya in wet years, fluctuating in salinity and flooding an area of up to 4500 km² in salt water to a depth of about one meter, which would preclude any economic activity in the area, while the western basin becomes increasingly saline. Water diversion from the Amu Darya directly to the deeper western basin could lower its salinity enough to allow resumption of local fisheries, while allowing the eastern basin to desiccate almost entirely and avoiding the problems of flooding.
The West Aral Sea is expected to stabilize at 2,700–3,500 km2 (1,040–1,350 sq mi), a mean depth of 14–15 m (46–49 ft), and a maximum depth of 37–40 m (121–131 ft), assuming groundwater discharge at the rate of 2 km3 (0.5 cu mi) per year. The Eastern Sea dried up completely in the summer of 2009, but it received some water from snow melt in the spring of 2010. It is expected to alternate between complete desiccation in the summers and the occasional flood from the Amu Darya or spillover from the dam holding back the North Aral Sea.
- "Seen from Space - South Aral Sea shrinking but North Aral Sea expanding". EORC. Retrieved 2013-09-01.
- Harald Frater. "scinexx | Aralsee: Ostbecken ist jetzt Wüste: Satellitenaufnahmen dokumentieren dramatische Austrocknung der letzen Jahre - Wüsten, Aralsee, Desertifikation, Wasser, Bewässerung, Landschaft, Landwirtschaft, Flüsse". Scinexx.de. Retrieved 2013-09-01.
- "Freshwater Ecoregions of the World". Feow.org. 2013-02-26. Retrieved 2013-09-01.
- "The Shrinking Aral Sea Recovers : Image of the Day". Earthobservatory.nasa.gov. doi:10.1111/j.1440-1770.2010.00437.x. Retrieved 2013-09-01.
- "Groundwater discharge into the Aral Sea after 1960". Sciencedirect.com. Retrieved 2013-09-01.
- Peter O. Zavialov, 2005, Physical oceanography of the dying Aral Sea, p 112
- "The rehabilitation of the ecosystem and bioproductivity of the Aral Sea under conditions of water scarcity" (rev. 2007 Aug.)