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The Irtysh River is a tributary of the Ob River.
The Irtysh River is the largest tributary of the Ob River and is known as the "Silver Water". International rivers flowing through China, Kazakhstan, Russia. The Irtysh River originates from the southern slope of the Altai Mountains in Fuyun County, Xinjiang Uygur Autonomous Region, China, flows northwest along the southern foot of the Altai Mountains, enters the state of Kazakhstan to the west of Haba County, and flows into Zaisangpo (now it flows into the Bukhtalma Reservoir after transit, and Zaisangpo has become part of the reservoir), and continues to flow northwest through northeast Kazakhstan after exiting the lake, and after entering Russia, it turns northeast through Omsk, turns northwest near Tara, and turns north at Tobolsk. It joins the Ob River near Khantymansiysk.
The Irtysh River is the only river that flows into the Arctic Ocean in China, originating from the southwest slope of the Altai Mountains in China. After the confluence of the Kayirt River and the Kuyirt River, it becomes the Irtysh River, which flows out of China from southeast to northwest, and merges the northern bank tributaries such as the Kara Irtysh River, the Klan River, the Burzin River, the Haba River, and the Berezek River along the way, flows into the Zaisan Lake in Kazakhstan, and then flows into the Arctic Ocean through the Ob River in the north through Russia. With a total length of 4,248 kilometers, 546 kilometers in China, the basin covers an area of 10,000 square kilometers, with an annual runoff of 11.1 billion cubic meters, ranking second only to the Ili River in Xinjiang, China.
It is known as the second largest river in Xinjiang. The water is abundant in fish, and the river is as wide as a kilometre near the border and accessible to ships. Many tributaries in the basin flow in from the right bank of the main stream, forming a typical comb-shaped water system.
The scenery along the Irtysh River is magnificent. It should also be known as "gold mountain" and "silver water".
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The Irtysh River is the largest tributary of the Ob River.
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Topography reasons.
According to the data of the question bank, the water system of the Irtysh River is "comb-shaped", indicating that the distribution of its tributaries is asymmetrical, and there is the Altai Mountains in the north of the socks basin of the river, which is high and blocks the westerly wind, forming rich topographic rain, so there are many tributaries on the right bank.
The Irtysh River is the largest tributary of the Ob River and is known as the "Silver Water". International rivers flowing through China, Kazakhstan, Russia. The Irtysh River originates from the southern slope of the Altai Mountains in Fuyun County, Xinjiang Uygur Autonomous Region, China, flows northwest along the southern foot of the Altai Mountains, enters the country of Kazakhstan in the west of Haba River County, flows into Zaisangbo, continues to flow northwest through the northeast of Kazakhstan after leaving the lake, enters Russia, turns to the northeast through the Hujiao Haohaomusk, turns to the northwest near Tara, turns to the north at Tobolsk, and joins the Ob River near Khantymansiysk.
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Hello, I'm glad to answer for you. The Irtysh River is a transnational river that originates in China's Xinjiang Uygur Autonomous Region, flows from southeast to northwest, and flows into tributaries along the way, eventually flowing into the Arctic Ocean, and is the only river in China that flows into the Arctic Ocean. It has a total length of 4,248 kilometers, a basin area of 10,000 square kilometers and a land mile, with an annual runoff of 11.1 billion cubic meters, second only to the Ili River in terms of water volume, ranking second in Xinjiang, China, and known as the second largest river in Xinjiang.
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Hydrological characteristics of the Irtysh River: the upper reaches are mainly fed by snowmelt, ice melt and precipitation; The downstream is mainly snowmelt, precipitation and soil water. The upstream flood season begins in April, and the major flood season is mostly in April and June. The downstream flood season is from the end of May to October, with the highest in June, accounting for about 50% of the year.
The upper reaches of the Irtysh River flow above Ust-Kamenogorsk between the Altai mountain ranges, with more precipitation, a well-developed river network, and abundant runoff; Passing through Ust-Kamenogorsk, the valley is open and a plain river.
The main tributaries that flow into the upper section are: Kurchum, Bukhtarma, Uriba, Uba, Kyzylsu and Char.
There are no major tributaries from Semipalatinsk to Omsk, and the river flows through the West Siberian Plain with twists and turns. The Omsk River turns sharply to the northeast, then to the northwest, and finally to the northeast to join the Ob River. The tributaries of this section are the Om, Ishim, Tobol, Demyyanka, Konda and others.
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The basin is mainly temperate continental climate, and the rivers are mainly fed by ice and snow meltwater and mountain precipitation, with small runoff and large seasonal variations. The winter temperature is low and long, the freezing period is long, and there is a flow interruption in winter.
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