Climate is found in south west Siberia and Eastern
Mangolia.
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- Temperature. The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold East Asia has a temperate climate. The highest temperature recorded in Asia was 54.0 °C (129.2 °F) at Tirat Zvi, Israel on June 21, 1942 and at Ahvaz, Iran on June 29, 2017.
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Southwest Siberia
Almost all the population lives in the south, along the route of the Trans-Siberian Railway. The climate in this southernmost part is Humid continental climate (Köppen Dfb) with cold winters but fairly warm summers lasting at least four months. The annual average temperature is about 0.5 °C (32.9 °F).
Eastern Mangolia
Mongolia has a high elevation, with a cold and dry climate. It has an extreme continental climate with long, cold winters and short summers, during which most precipitation falls. The country averages 257 cloudless days a year, and it is usually at the center of a region of high atmospheric pressure.
Climate: Desert; continental
Environmental issues: Limited natural freshwater
Terrain: Vast semidesert and desert plains
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