Tarim River

Chinese Talimu He or T'a-li-mu Ho

Chief river of Xinjiang autonomous region, China.

Formed by the confluence of two rivers in the far west, it follows an undefined riverbed for much of its course, flowing along the northern edge of the Takla Makan Desert before turning southeast. Because it frequently changes course, its length varies but is about 1,260 mi (2,030 km). The Tarim Basin is enclosed by the Tien Shan, the Pamirs, and the Kunlun Mountains. It is the driest region of Eurasia.

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▪ river, China

Chinese (Pinyin)  Talimu He  or  (Wade-Giles romanization)  T'a-li-mu Ho 

      chief river of the Uygur Autonomous Region of Xinjiang (Sinkiang, Uygur Autonomous Region of), extreme northwestern China. It lies immediately north of the Plateau of Tibet (Tibet, Plateau of). The river gives its name to the great basin between the Tien Shan and Kunlun (Kunlun Mountains) mountain systems of Central Asia (Central Asia, history of). It flows for most of its length through the Takla Makan Desert. The word tarim is used to designate the bank of a river that flows into a lake or that is undifferentiable from the sands of a desert. This is a characteristic hydrographic feature of many rivers that traverse the sands of the Takla Makan Desert. Another characteristic of the rivers of the Tarim Basin, including the Tarim itself, is their active migration—i.e., the shifting of their beds and banks.

      The Tarim is formed by the confluence of the Kaxgar (Kashgar) and Yarkand (Yarkand River) (Yarkant) rivers in the far west; flowing northeastward from this confluence, the river is then joined some 230 miles (370 km) downstream by the Aksu and the Hotan (Khotan) rivers. Only the Aksu River flows for the entire year. It is the Tarim's most important tributary, supplying 70–80 percent of its water volume. The name Tarim is used below the Hotan River confluence. The Tarim once reached Lop Nur, a large saline lake in eastern Xinjiang. However, reservoirs and irrigation works built along its middle course in the mid-20th century have diverted much of its waters. By the 1970s the combination of this water loss and the intense evaporation produced by the region's dry climate had dried up the Tarim's lower course, and Lop Nur had become a vast salt-encrusted lake bed. The Tarim also once fed Lake Taitema, located about 100 miles (160 km) southwest of Lop Nur, but the Daxihaizi dam and reservoir project built in the 1970s dried up the river downstream and the lake; the central government has had some success in restoring the river's flow below the reservoir.

      The total length of the Yarkand-Tarim river system prior to the 1970s was given as about 1,260 miles (2,030 km). However, a considerable part of the Tarim's course is unformed, following no clearly defined riverbed and frequently changing channels, and the river's length has varied over the years. The Tarim's low-water period is from October through April. The spring and summer high waters begin in May and continue through September as the snows melt on the distant Tien Shan and Kunlun mountains.

      The area drained by the Yarkand-Tarim system is about 215,000 square miles (557,000 square km), much of it comprising the Tarim Basin. The basin is an arid plain composed of alluvium and lake sediments and is bordered by massive mountain ranges. It is the driest region of Eurasia. The predominant part of it is occupied by the Takla Makan Desert, whose sand area exceeds 123,550 square miles (320,000 square km). In addition, there are several comparatively small sand massifs with areas of 300 to 1,700 square miles (780 to 4,400 square km). Sand dunes are the predominant landform.

      Precipitation in the Tarim Basin is extremely scanty, and in some years it is nonexistent. In the Takla Makan Desert and in the Lop Nur basin, the total average annual precipitation is about 0.5 inch (12 mm). In the foothills and in several other areas of the river's basin, the precipitation amounts to 2 to 4 inches (50 to 100 mm) a year. The slopes of the Tien Shan are much wetter, precipitation there often exceeding 20 inches (500 mm). Maximum temperatures in the Tarim Basin reach about 104 °F (40 °C). The Tarim River freezes over every year from December through March.

      Vegetation in the Tarim Basin is mainly located along the river and its branches. There, at the edge of the sands, are found shrublike vegetation and stunted trees, especially wormwood. A thin forest of diversiform-leaved poplar grows in the Tarim River valley. Underbrush consists of willows, sea buckthorn, and dense growths of Indian hemp and Ural licorice.

      The upper course of the Tarim River contains fish, and animal life on that portion of the river and in the desert is varied. The valley and lakes of the Tarim are a stopover for migratory birds.

      The migration of Chinese (Han) into the area and the Chinese government's promotion of large-scale irrigation have resulted in the spread of irrigation-based agriculture, but oasis agriculture continues in scattered Uighur settlements in the region. Rice and other grains, cotton, silk, fruits, and wool are the chief agricultural products, and Khotan jades and carpets are other important items. High-quality cotton and cotton cloth and several varieties of fruit, including watermelon and grapes, are exported from the region.

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