South Aral Sea

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South Aral Sea
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The Aral Sea in mid-August 2014. The two remaining lakes to the south and west are the remains of the South Aral Sea.
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South Aral Sea
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South Aral Sea
Location KazakhstanUzbekistan,
Central Asia
Coordinates 45°00′N58°30′E / 45°N 58.5°E / 45; 58.5
Type endorheic, natural lake
Primary inflows groundwater only
(previously the Amu Darya)
Basin  countriesKazakhstan, Uzbekistan
Surface areaWest Aral Sea:
3,500 km2 (1,350 sq mi) (2005)
(fluctuating area of Eastern Sea)
42,100 km2 (16,250 sq mi) (1989)
Average depth14–15 m (46–49 ft) (2005)
Max. depth37–40 m (121–131 ft) (2005)
Surface elevation29 m (95 ft) (2007)
References [1]

The South Aral Sea was a lake in the basin of the former Aral Sea which formed in 1987 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. [2] [3] In 2010, it was partially filled again by meltwater, [4] and by 2014 was once again dry. The West Aral Sea has some replenishment from groundwater in the northwest. [5]

Contents

Background

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 in order to irrigate cotton and food crops in Kazakhstan and Uzbekistan. In 1987, 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.

Salinity

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. [6] 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. [7]

Current situation

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. [6] The Eastern Sea dried up completely in the summer of 2009, apart from the small permanent Barsakelmes Lake (between the Northern and Western seas), 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, though a second dike, begun in 2010, may reduce the incidence of the latter.

In 2015, the Western Sea was starting to split into two, as the channel that connects the central part of the sea and the small North-Eastern part was growing skinnier. (This can be seen on the 2014 picture.) Since 2018, the split has been complete. [8] [9]

Related Research Articles

<span class="mw-page-title-main">Amu Darya</span> River in Central Asia

The Amu Darya, also called the Amu, the Amo, and historically the Oxus, is a major river in Central Asia and Afghanistan. Rising in the Pamir Mountains, north of the Hindu Kush, the Amu Darya is formed by the confluence of the Vakhsh and Panj rivers, in the Tigrovaya Balka Nature Reserve on the border between Afghanistan and Tajikistan, and flows from there north-westwards into the southern remnants of the Aral Sea. In its upper course, the river forms part of Afghanistan's northern border with Tajikistan, Uzbekistan, and Turkmenistan. In ancient history, the river was regarded as the boundary of Greater Iran with Turan, which roughly corresponded to present-day Central Asia. The Amu Darya has a flow of about 70 cubic kilometres per year on average.

<span class="mw-page-title-main">Geography of Kazakhstan</span> Overview of the geography of Kazakhstan

Kazakhstan is located in Central Asia. With an area of about 2,724,900 square kilometers (1,052,100 sq mi) Kazakhstan is more than twice the combined size of the other four Central Asian states and 60% larger than Alaska. The country borders Turkmenistan, Uzbekistan, and Kyrgyzstan to the south; Russia to the north; Russia and the Caspian Sea to the west; and China's Xinjiang Uygur Autonomous Region to the east.

<span class="mw-page-title-main">Geography of Tajikistan</span> Overview of the geography of Tajikistan

Tajikistan is nestled between Kyrgyzstan and Uzbekistan to the north and west, China to the east, and Afghanistan to the south. Mountains cover 93 percent of Tajikistan's surface area. The two principal ranges, the Pamir Mountains and the Alay Mountains, give rise to many glacier-fed streams and rivers, which have been used to irrigate farmlands since ancient times. Central Asia's other major mountain range, the Tian Shan, skirts northern Tajikistan. Mountainous terrain separates Tajikistan's two population centers, which are in the lowlands of the southern and northern sections of the country. Especially in areas of intensive agricultural and industrial activity, the Soviet Union's natural resource utilization policies left independent Tajikistan with a legacy of environmental problems.

<span class="mw-page-title-main">Geography of Turkmenistan</span> Overview of the geography of Turkmenistan

Turkmenistan is a landlocked country in Central Asia, bordering the Caspian Sea to the west, Iran and Afghanistan to the south, Uzbekistan to the north-east, and Kazakhstan to the north-west. It is the southernmost republic of the Commonwealth of Independent States (CIS), the loose federation created at the end of 1991 by most of the Post-Soviet states.

<span class="mw-page-title-main">Geography of Uzbekistan</span> Overview of the geography of Uzbekistan

Uzbekistan is a country in Central Asia, located north of Turkmenistan and Afghanistan. With an area of 447,000 square kilometers, Uzbekistan stretches 1,425 km (885 mi) from west to east and 930 km (580 mi) from north to south. It borders Turkmenistan to the southwest, Kazakhstan to the north and Tajikistan and Kyrgyzstan to the south and east. Uzbekistan also has four small exclaves in Turkmenistan.

<span class="mw-page-title-main">Aral Sea</span> Lake between Kazakhstan and Uzbekistan

The Aral Sea was an endorheic lake lying between Kazakhstan to its north and Uzbekistan to its south which began shrinking in the 1960s and largely dried up by the 2010s. It was in the Aktobe and Kyzylorda regions of Kazakhstan and the Karakalpakstan autonomous region of Uzbekistan. The name roughly translates from Mongolic and Turkic languages to "Sea of Islands", a reference to the large number of islands that once dotted its waters. The Aral Sea drainage basin encompasses Uzbekistan and parts of Afghanistan, Iran, Kazakhstan, Kyrgyzstan, Tajikistan, and Turkmenistan.

<span class="mw-page-title-main">Karakum Desert</span> Desert in Central Asia

The Karakum Desert, also spelled Kara-Kum and Gara-Gum, is a desert in Central Asia. The name refers to the shale-rich sand beneath the surface. It occupies about 70 percent, or roughly 350,000 km2 (140,000 sq mi), of Turkmenistan.

<span class="mw-page-title-main">Endorheic basin</span> Closed drainage basin that allows no outflow

An endorheic basin is a drainage basin that normally retains water and allows no outflow to other, external bodies of water ; instead, the water drainage flows into permanent and seasonal lakes and swamps that equilibrate through evaporation. Endorheic basins also are called closed basins, terminal basins, and internal drainage systems.

<span class="mw-page-title-main">Lake Balkhash</span> Lake in southeastern Kazakhstan

Lake Balkhash is a lake in southeastern Kazakhstan, one of the largest lakes in Asia and the 15th largest in the world. It is located in the eastern part of Central Asia and sits in the Balkhash-Alakol Basin, an endorheic (closed) basin. The basin drains seven rivers, the primary of which is the Ili, bringing most of the riparian inflow; others, such as the Karatal, bring surface and subsurface flow. The Ili is fed by precipitation, largely vernal snowmelt, from the mountains of China's Xinjiang region.

<span class="mw-page-title-main">Salt lake</span> Landlocked body of water which has a high concentration of salts

A salt lake or saline lake is a landlocked body of water that has a concentration of salts and other dissolved minerals significantly higher than most lakes. In some cases, salt lakes have a higher concentration of salt than sea water; such lakes can also be termed hypersaline lakes, and may also be pink lakes on account of their colour. An alkalic salt lake that has a high content of carbonate is sometimes termed a soda lake.

<span class="mw-page-title-main">Moynaq</span> Town in Karakalpakstan, Uzbekistan

Moynaq, also spelled as Muynak, is a city in northern Karakalpakstan, an autonomous republic in Uzbekistan. It is the seat of the Moynaq district. Formerly a sea port on the Aral Sea, it is now 150 km from the water in the Aralkum Desert and thus is a disaster tourism destination. It is also the location for the biggest electronic music festival in Central Asia.

<span class="mw-page-title-main">Messinian salinity crisis</span> Drying-up of the Mediterranean Sea from 5.96 to 5.33 million years ago

The Messinian salinity crisis was a geological event during which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation (drying-up) throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma. It ended with the Zanclean flood, when the Atlantic reclaimed the basin.

<span class="mw-page-title-main">North Aral Sea</span> Extant lake

The North Aral Sea is the portion of the former Aral Sea that is fed by the Syr Darya River. It split from the South Aral Sea in 1987–1988 as water levels dropped due to river diversion for agriculture.

<span class="mw-page-title-main">Sarygamysh Lake</span> Lake in Central Asia

The Sarygamysh Lake, also Sarykamysh or Sary-Kamysh, is a lake in Central Asia. It is about midway between the Caspian Sea and the Aral Sea. It is the largest lake in Turkmenistan, in which three quarters of the entire lake's area is located. The Sarykamysh basin and the Sarykamysh delta of the Amu Darya river are physical and geographical nature regions of the Dashoguz Region of Turkmenistan.

<span class="mw-page-title-main">Aydar Lake</span> Artificial lake in Kyzyl Kum

The Aydar Lake is part of the man-made Aydar-Arnasay system of lakes, which covers 4,000 square kilometres (1,500 mi2). This has 3 brackish water lakes, deep basins of the south-eastern Kyzyl Kum. The lakes are expansive reservoirs of Soviet planning.

<span class="mw-page-title-main">Kamyslybas</span> Lake in Kazakhstan

Kamyslybas is a large saltwater lake in the Kyzylorda Region, Kazakhstan. It has an area of 176 km2, although the water level in the lake often fluctuates.

Environmental issues in Turkmenistan are most visible in three significant areas: desertification, the drying of the Aral Sea, and chemical pollution. All three of these areas are directly linked to agricultural practices in the country.

<span class="mw-page-title-main">Uzboy</span> Former river in west Asia

The Uzboy was a distributary of the Amu Darya which flowed through the northwestern part of the Karakum Desert of Turkmenistan until the 17th century, when it abruptly dried up, eliminating the agricultural population that had thrived along its banks..

<span class="mw-page-title-main">Endorheic lake</span> Depression within an endorheic basin where water collects with no visible outlet

An endorheic lake is a collection of water within an endorheic basin, or sink, with no evident outlet. Endorheic lakes are generally saline as a result of being unable to get rid of solutes left in the lake by evaporation. These lakes can be used as indicators of anthropogenic change, such as irrigation or climate change, in the areas surrounding them. Lakes with subsurface drainage are considered cryptorheic.

<span class="mw-page-title-main">Central Asian riparian woodlands</span>

The Central Asian riparian woodlands ecoregion is spread out across the deserts and plains of central Asia between the Aral Sea and the mountains 2,000 kilometres (1,200 mi) to the east. The long narrow components of the ecoregion follow the large rivers fed by snowmelt, and provide critical habitat for migratory birds as they travel through the arid region. The vegetation is referred to as tugai, characterized by low tangles of trees and brush along the edges of the rivers and associated wetlands, and fed by groundwater instead of precipitation.

References

  1. "Seen from Space – South Aral Sea shrinking but North Aral Sea expanding". EORC. Retrieved 31 May 2017.
  2. Harald Frater (10 August 2009). "scinexx | Aralsee: Ostbecken ist jetzt Wüste: Satellitenaufnahmen dokumentieren dramatische Austrocknung der letzen Jahre – Wüsten, Aralsee, Desertifikation, Wasser, Bewässerung, Landschaft, Landwirtschaft, Flüsse". Scinexx.de. Retrieved 1 September 2013.
  3. "Freshwater Ecoregions of the World". Feow.org. 26 February 2013. Archived from the original on 19 February 2012. Retrieved 1 September 2013.
  4. "The Shrinking Aral Sea Recovers : Image of the Day". Earthobservatory.nasa.gov. 30 October 2010. doi:10.1111/j.1440-1770.2010.00437.x . Retrieved 1 September 2013.{{cite journal}}: Cite journal requires |journal= (help)
  5. Jarsjö, Jerker; Destouni, Georgia (2004). "Groundwater discharge into the Aral Sea after 1960". Journal of Marine Systems. 47 (1–4): 109–120. Bibcode:2004JMS....47..109J. doi:10.1016/j.jmarsys.2003.12.013.
  6. 1 2 Peter O. Zavialov, 2005, Physical oceanography of the dying Aral Sea, p 112
  7. "The rehabilitation of the ecosystem and bioproductivity of the Aral Sea under conditions of water scarcity" (rev. August 2007)
  8. https://www.weforum.org/agenda/2020/02/aral-sea-lake-water-nature-human-impact/ Satellite image of 2018
  9. https://eurasianet.org/northern-arals-promise-stunted-by-dam-height-international-disputes Satellite image of 2020