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- North Asia is a subregion of Eurasia, consisting of the Asian territory of Russia, includes the Urals, Siberia and the Far East. The climate in the north of Asia is continental with a pronounced contrast of temperatures and very cold winters.
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Asia is dominated by a varied mix of climate regions. Polar, subarctic, and temperate climates occur along the continent's northern and northeastern fringes; arid and highland climates occur in the continent's interior and southwestern reaches; and a mix of grassland and tropical rainforest climates occur along its southern fringe.
Especially in the Pacific region of Asia, ocean currents are responsible for strong or less pronounced rainy seasons. Mountains are also a frequent weather divide. For example, there is always a different climate north and south of the Alpine ridge or on both sides of the American Rocky Mountains.
The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold, and East Asia has a temperate climate. The highest temperature recorded in Asia was 61.36 °C in Multan, Punjab, Pakistan on July 26, 1992. [2]
- Tundra Region: It spans the entire continent from east to west along the Arctic Ocean and includes the lowlands between the Arctic Circle and 70°N, the southern limits roughly coincide with the July isotherm of 50°F (10°C).
- East Siberia: ADVERTISEMENTS: Between 50° and 70°N latitudes a large territory in eastern Siberia including the lower basin of Lena river and the area to the north of Baikal lake.
- West Siberia: The region is located west of the preceding region all the way to the Ural Mountains. Temperatures are higher than in East Siberia, and there is a little more rainfall (up to 250 mm annually)—a clear evidence of the Pacific influence.
- Temperate Monsoon Lands of East Asia: Most of eastern China, North Korea, South Korea, and Japan are included in this region which lies entirely north of the Tropic of Cancer.
The climate in West Siberia (Omsk, or Novosibirsk) is several degrees warmer than in the East (Irkutsk, or Chita) where in the north an extreme winter subarctic climate (Köppen Dfd, Dwd, or Dsd) prevails. But summer temperatures in other regions can reach +38 °C (100 °F).
North Asia is a subregion of Eurasia, consisting of the Asian territory of Russia, includes the Urals, Siberia and the Far East. The climate in the north of Asia is continental with a pronounced contrast of temperatures and very cold winters. North-Asian Regions
