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- Once the fourth largest lake in the world, Central Asia's shrinking Aral Sea has reached a new low, thanks to decades-old water diversions for irrigation and a more recent drought. Satellite imagery released this week by NASA shows that the eastern basin of the freshwater body is now completely dry.
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Find out the answer to the crossword puzzle clue \"Shrinking Asian sea\" and see related clues and recent usage. The answer is Aral Sea, a landlocked lake in Central Asia that has dried up due to human activities.
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- Overview
- Geology
- Climate and hydrology
- Physiographic changes
The Aral Sea stands at the boundary between Kazakhstan to the north and Uzbekistan to the south. It was once a large saltwater lake of Central Asia and the world’s fourth largest body of inland water.
Why has the Aral Sea been shrinking?
The primary cause behind the shrinking of the Aral Sea is the diversion (for purposes of irrigation) of the main sources of inflowing water, the riverine waters of the Syr Darya (ancient Jaxartes River) in the north and the Amu Darya (ancient Oxus River) in the south, which historically discharged into the Aral Sea.
How deep was the Aral Sea?
The average depth of the Aral Sea was a relatively shallow 53 feet (16 meters) or so. It descended to a maximum of 226 feet (69 meters) off the western shore.
How big was the Aral Sea originally?
The Aral Sea depression was formed toward the end of the Neogene Period (which lasted from about 23 to 2.6 million years ago). Sometime during that process the hollow was partially filled with water—a portion of which came from the Syr Darya. In the early and middle parts of the Pleistocene Epoch (about 2,600,000 to 11,700 years ago), the region ap...
The Aral Sea area is characterized by a desert-continental climate that features wide-ranging diurnal air temperatures, cold winters, hot summers, and sparse rainfall. The rate of precipitation—an annual average of 4 inches (100 mm) in all, occurring mainly in the spring and autumn—is only a tiny fraction of the lake’s traditional rate of evaporation. Northwesterly winds prevail in autumn and winter, and westerly and southwesterly winds are common in spring and summer.
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Until the 1960s the most-significant factors affecting the water balance of the Aral Sea were the rates of river inflow and water loss through evaporation, which formerly took out each year about the same amount of water that the rivers brought in. Over the centuries, variations in the water level exceeded 20 feet (6 metres), while annual and seasonal variations of between 10 feet (3 metres) and less than 1 foot (0.3 metre) were recorded.
In 1960 the surface of the Aral Sea lay 175 feet (53 metres) above sea level and covered an area of some 26,300 square miles (68,000 square km). The Aral Sea’s greatest extent from north to south was almost 270 miles (435 km), while from east to west it was just over 180 miles (290 km). Although the average depth was a relatively shallow 53 feet (16 metres) or so, it descended to a maximum of 226 feet (69 metres) off the western shore. The sea’s northern shore—high in some places, low in others—was indented by several large bays. The low-lying and irregular eastern shores were interrupted in the north by the huge delta of the Syr Darya and were bordered in the south by a wide tract of shallow water. The equally vast Amu Darya delta lay on the lake’s southern shore, and along the lake’s western periphery extended the almost unbroken eastern edge of the 820-foot- (250-metre-) high Ustyurt Plateau.
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Beginning about 1960, the Aral Sea’s water level was systematically and drastically reduced, because of the diversion of water from the Amu Darya and Syr Darya rivers for purposes of agricultural irrigation. As the Soviet government converted large acreages of pastures or untilled lands in what are now Uzbekistan, Kazakhstan, Turkmenistan, and elsewhere in Central Asia into irrigated farmlands by using the waters of the Amu Darya, Syr Darya, and their tributaries, the amount of water from those rivers that reached the Aral Sea dropped accordingly. By the 1980s, during the summer months, the two great rivers virtually dried up before they reached the lake. The Aral Sea began to quickly shrink because of the evaporation of its now unreplenished waters.
By 1989 the Aral Sea had receded to form two separate parts, the “Greater Sea” in the south and the “Lesser Sea” in the north, each of which had a salinity almost triple that of the sea in the 1950s. By 1992 the total area of the two parts of the Aral Sea had been reduced to approximately 13,000 square miles (33,800 square km), and the mean surface level had dropped by about 50 feet (15 metres). The governments of the states surrounding the Aral Sea tried to institute policies to encourage less water-intensive agricultural practices in the regions south and east of the lake, thus freeing more of the waters of the Amu Darya and the Syr Darya to flow into the lake and to stabilize its water level. Those policies succeeded in reducing water usage somewhat but not to the level necessary to have a significant impact on the amount of water reaching the Aral Sea. In 1994 those same states—Kazakhstan, Turkmenistan, and Uzbekistan, with the addition of Kyrgyzstan and Tajikistan—established a joint committee to coordinate efforts to save the Aral Sea. The difficulty of coordinating any plan between those competing states, however, hampered progress.
By the end of the century the Aral Sea had receded into three separate lakes: the Greater Sea had divided into a long, narrow, western lake and a larger, broader, eastern lake, with the remains of the Lesser Sea to the north. The water level had dropped to 125 feet (36 metres) above sea level, and the water volume was reduced by three-fourths of what it had been in 1960. Almost no water from the Amu Darya and the Syr Darya ever reached the Aral Sea anymore. In the early 21st century the eastern portion of the Aral Sea suffered the most drastic and immediate decline—diminishing by some four-fifths between 2006 and 2009. The World Bank funded the construction of the Kok-Aral Dam (completed 2005) and projects along the Syr Darya that appeared to be preserving the northern portion of the sea. However, the southern portion—both the eastern and western lobes but most notably the eastern—continued to shrink, despite some inflow of water from the north. For periods of time after 2010, the eastern lobe dried up altogether.
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Oct 2, 2014 · Once the fourth largest lake in the world, Central Asia's shrinking Aral Sea has reached a new low, thanks to decades-old water diversions for irrigation and a more recent drought....
Well, in Central Asia, to the east of the Caspian Sea, there's a clear reminder of what we can do the natural world. Shrinking sea. In the 1960s, the Aral Sea was the fourth-largest body of inland water on Earth. Just decades later, it was almost gone.
The Aral Sea ( / ˈærəl /) [4] [a] 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.
Oct 7, 2022 · However, the Caspian Sea is rapidly shrinking. On September 19, 2022, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite acquired this natural-color image (right) of the northern Caspian Sea.
