Whether the Tarim River is an endorheic or an outflow river

The Tarim River is the longest inland river in China.

Tarim River, which is located in the Tarim Basin, Xinjiang Uygur Autonomous Region.

Northern. The Tarim River originates in the Tien Shan Mountains.

and the Karakoram Mountains, along the Taklamakan Desert.

On the northern rim, it flows into Lake Taitma.

The area around the Tarim River has become an oasis because of the water of the Tarim River.

The Tarim River basin is far from the sea and deep in Central Asia.

Inland, surrounded by high mountains, the continental climate is very obvious, precipitation is scarce, evaporation is strong, the sunshine hours are long, the climate of the four seasons is very different, and the climate change is drastic.

The Tarim River Basin is deep inland, far from the ocean, surrounded by high mountains, water vapor is difficult to enter, precipitation is scarce, but evaporation is strong, and the water source is mainly meltwater from the surrounding high mountains ice and snow.

Most sections of the Tarim River are waterless in autumn and winter, and are seasonal rivers.

The water source of the Tarim River mainly comes from the ice and snow melt water of the Tianshan Mountains, Kunlun Mountains and other high mountains, so the flood season is mainly in the spring and summer, especially in the summer, the river has the largest water volume.

Along the Tarim River, there is a break in the downstream flow and desertification caused by excessive water diversion, and a large area of poplar forest has died.

The state is rationally allocating the water resources of the Tarim River, building water conservancy projects, and from Bosten Lake.

Water was diverted to support the Tarim River.

We know that outflow rivers will eventually flow into the ocean, so what about those inflow rivers that do not flow into the ocean and end up flowing to **?

Let's take the Tarim River, the longest inland river in our country, as an example. The Tarim River is located in the northwest region of China.

In the Tarim Basin, due to its inland location and distance from the sea, it is difficult for ocean moisture to reach, plus the surrounding Tianshan Mountains and Kunlun Mountains.

The climate is very arid, with annual precipitation of less than 100 mm and annual evaporation of more than 2,000 mm.

Therefore, it is impossible to form rivers in the Tarim Basin by relying on atmospheric precipitation.

The Tarim River is an inland river.

Rivers can be divided into two categories, outflow rivers and inflow rivers, according to their final destination. Those rivers that flow directly or indirectly into the ocean are called outflow rivers. Outflow rivers are generally located in the continental marginal areas with a relatively humid climate, abundant precipitation, low evaporation, and close to the sea.

More than 2 out of 3 of the world's rivers are outflow rivers. For example, the Amazon River in South America, the Nile River in Africa, the Yangtze River and the Yellow River in China, and the Mississippi River in Beijing and the Americas are all outflow rivers.

Those rivers that do not eventually flow into the ocean are called endorebic rivers, also known as inland rivers. Inland rivers are generally located in the interior of the continent far from the ocean. The climate there is often relatively dry, the precipitation is less, the water supply is insufficient, coupled with the strong sunshine, evaporation and other reasons, some rivers are injected into the inland lakes, and most of the remaining inland rivers are the Volga River in Russia, with a total length of 3,690 kilometers, and the river water is mainly fed by the melting snow water in the upper alpine regions, and finally flows into the world's largest lake - the Caspian Sea.

China's largest inland river is the Tarim River in Xinjiang, with a total length of more than 2,000 kilometers, and the river water is also fed by the ice water melted in the mountains, so the flow is larger in summer and less in winter, it flows through the Taklamakan Desert and finally flows into Lake Taitma.

The Tarim River, in the Uyghur language, means "horseless horse" and "field, farming". It is located in the northern part of the Tarim Basin, Xinjiang Uygur Autonomous Region. It originates from the Tianshan Mountains and the Karakoram Mountains, along the northern edge of the Taklamakan Desert, passes through the southern part of Aksu, Shaya, Kuqa, Luntai, Korla, Yuli and other counties (cities), and finally flows into Taitma Lake.

The main trunk of the Tahe River was first injected into Lop Nur, and then diverted due to the decrease in the amount of water in the river and the swing of the river channel, and the tail water reached the Taitema Lake in the north of Ruoqiang County before 1972, and the end point further retreated to the Daxihaizi Reservoir in Tieganlik. At the beginning of the 21st century, after the whole basin was controlled, the water began to flow back to Lake Taitma. The Tarim River is the mother river in southern Xinjiang, and the oases south of the Tianshan Mountains are basically irrigated by the Tarim River.

The Tarim River has a basin area of 1.02 million square kilometers. With a total length of 2,179 kilometers (some say, if the longest tributary, the Hetian River, is the source, the total length is 2,376 kilometers), it is the longest inland river in China and the fifth largest inland river in the world.

Inland rivers. The Tarim River is the longest inland river in China, and it is mainly located in the Tarim Basin of Xinjiang.

The main reasons for the interruption of the flow of the lower Tarim River are:

1. The natural reason for the interruption of the flow of the lower reaches of the Tarim River: The Tarim River flows through arid areas, and its water source mainly comes from the melting water of ice and snow in the mountains. As the river water flows forward, part of the water evaporates and some of the water seeps into the ground along the way, resulting in a continuous decrease in the volume of the Tarim River and a cut off in the downstream areas.

In recent decades, the warming climate has reduced the amount of snow and ice reserves in the mountains, the amount of water supplied to the rivers has decreased, and the evaporation has been intense, and a large amount of river water has been quickly lost, and the downstream of the river has been cut off.

2. Man-made reasons for the interruption of the flow in the lower reaches of the Tarim River: with the increase of population in the Tarim River Basin, large-scale reclamation and economic development have destroyed vegetation on the one hand, and the ability of vegetation to conserve water has declined; On the one hand, the amount of water used for agricultural irrigation has increased dramatically, and the people's domestic water consumption has increased significantly. A large amount of water from the Tarim Paiwei Canal was diverted, causing the river to reduce rapidly, and the river was cut off due to the lack of water supply in the lower reaches.

The decisive factor for the interruption of the flow of the lower reaches of the Tarim River is the anthropogenic factor.

3. The Tarim River is located in the inland area, the precipitation is scarce, and it is not suitable to vigorously develop planting and afforestation, so the industrial structure should be adjusted and water-saving agriculture should be developed.

The Tarim River is the largest inland river in China.

The Tarim River is formed by the confluence of the Aksu River, which originates in the Tianshan Mountains, the Yarkand River, and the Hotan River, which originates in the Karakoram Mountains, with a basin area of 10,000 square kilometers, and finally flows into Lake Taitma. It is the largest inland river in China, with a total length of 2,137 kilometers, second only to the Volga River in the former Soviet Union, the Syr-Narun River, the Amu Penchi-Vakhsh River and the Ural River, making it the fifth largest inland river in the world and the longest inland river in China.

In the northern part of the Tarim Basin, Xinjiang Uygur Autonomous Region. Historically, the course of the Tarim River swayed from north to south, and migration was uncertain. The last time in 1921 was that the main stream flowed east into the Peacock River and into Lop Nur.

In 1952, a dam was built near Yuli County, separated from the Peacock River, and the river water flowed to Taitma Lake through the Tieganlik Old Road.

Water conservancy facilities of the Tarim River:

The flow of the Tarim River varies greatly depending on the season. In the scorching summer months, when the snow and glaciers melt and the river flow increases dramatically, it is like a "wild horse without borders" galloping and roaring through the desert and grassland. There is an 80-hole, concrete structure and a bridge with a total length of more than 1,600 meters on the Tahe River.

Many water conservancy facilities have been built in the Tahe River basin. With the hard work of the people of all ethnic groups, the desert of the past has become a mulberry field, and the melons and fruits on both sides of the Tahe River are full of orchards, and the rice flowers are fragrant.

There are glaciers in the source area of the Tarim River, and the river water is ice and snow melt water and rainwater, and the water production is relatively abundant, and the interannual variation of water volume is small, which provides better conditions for the development of agriculture, forestry and animal husbandry along the river. Since 1958, 286 aqueducts of various types have been built, with a designed water diversion capacity of 882 m s.

Answer]: True. The Qilimu River of Seexiang Taling is formed by the confluence of the Aksu River, the Yarkand River and the Hotan River, and finally flows into the Taitema Lake, with a total length of 2,137 kilometers, which is the largest inland river in China and the fifth largest inland river in the world.

The Tarim River, the longest inland river in China.