South Aral Sea

South Aral Sea
The Aral Sea in mid-August 2014. The two remaining lakes to the south and west are the remains of the South Aral Sea.
Location	Kazakhstan–Uzbekistan, Central Asia
Coordinates	45°00′N 58°30′E / 45°N 58.5°E / 45; 58.5Coordinates: 45°00′N 58°30′E / 45°N 58.5°E / 45; 58.5
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)
References

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 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 almost completely dried out, leaving only the small permanent Barsakelmes Lake between the Northern and Western Seas and increasing the expanse of the Aralkum desert. In 2010, it was partially filled again by meltwater, and by 2014 was once again dry. 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.