The lowest temperature in Inner Mongolia.

The lowest historical temperature in Inner Mongolia is -50.8℃.

Genhe city, Inner Mongolia is located in the north of Hulunbeier, Inner Mongolia, and the north of Linhai, Daxinganling. It is one of the earliest places in China to start heating. Heating starts in September 1 every year, and the heating period lasts for 9 months. In September, the Genhe River was already sunny and "frozen", and the lowest temperature was below-10℃.

The annual extreme minimum temperature here can reach-50.8℃, and there are many extremely cold days (the daily minimum temperature is ≤-40℃), which lasts for a long time. There have also been years when the number of extremely cold days reached 69 days, and the longest continuous extremely cold days reached 27 days. Due to the continuous occurrence of extremely cold days in genhe city, the extreme average minimum temperature in winter and June is 5438+ 10, which is the highest in China, and it was awarded the title of "China Cold Pole" by the National Climate Center.

Climatic characteristics of Inner Mongolia

Inner Mongolia Autonomous Region is located in the southeast of Mongolian Plateau in Central Asia and its surrounding areas. Mainly plateau, with an altitude of 1000 meters above sea level, collectively referred to as Inner Mongolia Plateau. However, the internal landform structure is obviously different, including mountains, hills, plateaus, plains, deserts, Gobi and other landforms.

Because it is located in the middle latitude inland, most of it belongs to temperate continental monsoon climate, and only the northern part of Daxing 'anling belongs to cold temperate continental monsoon climate. The whole year is controlled by westerly circulation, mainly influenced by mid-latitude weather system, and the influence of monsoon circulation depends on seasonal changes. The influence time of winter monsoon is long, and that of summer monsoon is difficult to reach and short.

Its main climatic characteristics are: long and cold winter, strong wind and little rain in spring, short and warm summer, and sudden drop of temperature in autumn; Large temperature difference between day and night, sufficient sunshine time, large precipitation variability and short frost-free period. The temperature distribution increases from Daxinganling to the southeast and southwest.

Precipitation is scarce in most areas, concentrated in summer. The distribution of annual precipitation is contrary to the temperature, thus forming an unbalanced pattern of water and heat distribution in areas with the most heat and the least precipitation and heat.

Reference to the above content: Baidu Encyclopedia-Inner Mongolia Autonomous Region