Aral Sea
Topic: World Physical Features and Natural Regions · NCERT: Beyond NCERT
Meaning
The Aral Sea is a saltwater lake in a closed basin on the Kazakhstan–Uzbekistan border. It was once about 68,000 sq km, the 4th-largest lake in the world [1]. Since the 1960s it has shrunk to only about 10% of its 1960 size [1], because Soviet projects took water from its two feeder rivers, the Amu Darya and Syr Darya, to grow cotton.
It is one of the world's worst human-made environmental disasters. UPSC uses it as a classic case of poor water management, along with Lake Chad.
Explanation
Why the Aral is a closed lake
- The Aral Sea sits in an endorheic (closed) basin. This is a basin with no outlet to the ocean.
- How water comes in: almost all of it comes from two rivers:
- the Amu Darya
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the Syr Darya
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How water goes out: only by evaporation, because no river flows out to the sea.
- What this means:
- When water evaporates, the salt stays behind. Over time the lake becomes saline (salty).
- The lake stays the same size only while inflow from the rivers equals the water lost to evaporation.
- If inflow falls, the lake shrinks and gets saltier.
How the sea shrank (cause → process → result)
- Cause: river water was taken for cotton
- From the 1960s, Soviet projects took water from the Amu Darya and Syr Darya.
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The water went to irrigate cotton fields in the dry lands of Central Asia.
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Process: evaporation became greater than inflow
- Much less river water reached the sea.
- In this dry region, evaporation went on as before.
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So the sea lost more water each year than it received.
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Result: the sea shrank and split
- The sea is now only about 10% of its 1960 size [1].
- It has split into two parts: the North Aral (in Kazakhstan) and the South Aral [2].
Effects of the drying
- Aralkum desert: the dry seabed has become the Aralkum, a new toxic desert.
- Poisonous dust storms: winds lift salt and pesticide dust from the old seabed and carry it over nearby land and towns.
- Loss of livelihoods: fishing towns that once stood on the shore collapsed.
- Health and migration: the toxic dust harms people's health, and people leave the region to find work.
Partial recovery and its trade-off
- Kok-Aral Dam (Kazakhstan):
- Completed in 2005, it holds water back in the North Aral [2].
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It replaced an earlier dike built in the 1990s [2].
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Good result in the North:
- By 2011, the North Aral's salinity was back to its 1960s level of about 8 g per litre [2].
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Its fisheries have recovered [2].
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Cost in the South:
- The dam lets less water flow on to the south.
- So the South Aral keeps shrinking and getting saltier [1][2].
Where it occurs
- Location: Central Asia, on the Kazakhstan–Uzbekistan border [1].
- Feeder rivers: the Amu Darya and the Syr Darya. Their water was diverted for cotton irrigation.
- Present parts:
- North Aral: in Kazakhstan. It is held back by the Kok-Aral Dam (2005) and is recovering [2].
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South Aral: it is still shrinking and getting saltier [1][2].
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Aralkum: the new toxic desert on the dried seabed.
- A similar case in the world: Lake Chad in the Sahel (Chad, Cameroon, Niger, Nigeria) has also shrunk by more than 90% since the 1960s [3].
- Lesson for India: shrinking lakes such as Sambhar and Loktak show the same risk. Both need basin-level planning and control over how much water is used.
Don't confuse with
- Caspian Sea: the world's largest inland water body (about 371,000 sq km), fed mainly by the Volga. It is shrinking mainly because the Volga brings less water and a warming climate raises evaporation. The Aral shrank mainly because people diverted its rivers for cotton.
- Lake Chad: it also shrank by more than 90%, but the main cause was less rain where its feeder rivers, the Chari and Logone, begin [3]. Irrigation was only a secondary cause. The Aral's main cause was irrigation diversion.
- Lake Balkhash: also in Kazakhstan, fed by the Ili River. It is half fresh (west) and half salty (east). The Aral is not divided this way. It split into a North and a South part because it shrank.
- North Aral vs South Aral: the Kok-Aral Dam (2005) saved the North Aral (Kazakhstan). It did not save the South Aral, which is still drying.
Prelims Hooks
- Aral Sea – feeder rivers: Amu Darya and Syr Darya (not the Volga, which feeds the Caspian).
- Location: Kazakhstan–Uzbekistan border. It was once the 4th-largest lake in the world, at about 68,000 sq km [1].
- Cause of shrinking: Soviet diversion of river water for cotton irrigation from the 1960s. The sea is now about 10% of its 1960 size [1].
- Trap: the Kok-Aral Dam (2005) is in Kazakhstan and saved the North Aral, not the South Aral [2].
- Aralkum is the toxic desert that formed on the dried bed of the Aral Sea.
- Classification: the Aral is an endorheic (closed) basin lake, like the Caspian, the Dead Sea, the Great Salt Lake and Lake Chad.
Mains Points
- Human-made drying (GS-I/III): taking too much river water for cotton made the Aral Sea shrink to about 10% of its 1960 size [1].
- Effects: toxic salt-and-pesticide dust storms from the Aralkum, collapse of fisheries, harm to people's health, and migration.
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Lake Chad (drought plus irrigation) shows the same pattern of about 90% shrinking, with food insecurity and the growth of Boko Haram.
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Recovery is possible but has trade-offs: the Kok-Aral Dam brought salinity in the North Aral back to about 8 g per litre by 2011 and revived its fisheries [2]. The South Aral was left to keep drying [1][2]. Restoration often means choosing which part to save.
- Lesson for India (GS-III): plan for whole river basins and control the demand for water, not just the supply. Shrinking lakes such as Sambhar and Loktak need this approach before they reach an Aral-like state.
Related concepts
Read more
Sources
- 1Aral Sea, Kazakhstan and Uzbekistan — USGS EROS Earthshotseros.usgs.gov · tier 2
- 2Kok-Aral Dam — USGS EROS Earthshotseros.usgs.gov · tier 2
- 3Lake Chad facing humanitarian disaster — FAO Newsroomfao.org · tier 2