Climate
The climate of Ural is continental. The ridges of the Ural Mountains are elongated from north to south, they effectively absorb sunlight thereby increasing the temperature. The areas west to the Ural Mountains are 1–2 °C warmer in winter than the eastern regions because the former are warmed by the Atlantic winds whereas the eastern slopes are chilled by the Siberian air masses. The average January temperatures increase in the western areas from –20 °C in the Polar to –15 °C in the Southern Urals and the corresponding temperatures in July are 10 °C and 20 °C. The western areas also received more rainfall than the eastern ones by 150–300 mm per year. The highest precipitation (1000 mm) is in the Northern Ural that causes the average height of snow up to 90 cm. The eastern parts receive from 500–600 mm on the north to 300–400 mm on the south.
Read more about this topic: Ural (region)
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