What is the temperature throughout the year in Inner Mongolia?

Inner Mongolia has a typical mid-temperate monsoon climate, with notable characteristics of low and uneven precipitation and dramatic changes in cold and heat. Winter is long and cold, and the cold season lasts from 5 months to half a year in most areas. January is the coldest month, with the average monthly temperature decreasing from minus 10 degrees Celsius to minus 32 degrees Celsius from south to north. The summer is warm and short, lasting only one to two months in most areas, and there is no summer in some areas. The hottest month is July, with the average monthly temperature ranging from 16℃ to 27℃ and the highest temperature from 36℃ to 43℃. The temperature changes drastically, and the difference between cold and warm is huge. The amount of precipitation is affected by the topography and the distance of the ocean, and decreases from 500 mm to about 50 mm from east to west. The amount of evaporation is the opposite, decreasing from 3000 mm to about 1000 mm from west to east. The corresponding climate zones are distributed in strips, gradually transitioning from humid and semi-humid areas to semi-arid and arid areas from east to west. There are many sunny days and few cloudy days here, and the sunshine hours are generally more than 2,700 hours, and the longest one is 3,400 hours. It is windy in winter and spring, with the annual average wind speed above 3 meters/second, and it contains rich light, heat and wind energy resources. Among them, Urad Middle Banner, located in Bayannur League, has more than 272 windy days throughout the year, making it one of the regions with the richest wind energy in the country.

Baotou is located in the west of the Inner Mongolia Autonomous Region, at the intersection of the Bohai Economic Zone and the resource-rich area in the upper reaches of the Yellow River. It borders Mongolia to the north, the Yellow River to the south, and the fertile Tumochuan Plain and Hetao Plain to the east and west. , the Yinshan Mountains run across the central part. The geographical coordinates of Baotou are 109°50' to 111°25' east longitude, 41°20' to 42°40' north latitude, and its area is 27,691 square kilometers.

Baotou includes Daqing Mountain and Wula Mountain (bounded by the Kundulun River) in the Yinshan Mountains. The average altitude of the peaks is 2,000 meters, and the highest peak is 2,324 meters above sea level. The city is composed of three parts: the central mountainous area, the northern mountain plateau grassland and the southern plain. The terrain is high in the middle, low in the north and south, and high in the west and low in the east. The Yellow River flows through Baotou City for 214 kilometers, with two highway and railway bridges flying parallel to the north and south of the Yellow River.

Baotou has a semi-arid mid-temperate continental monsoon climate. The scenery here is pleasant and the temperature is moderate. According to the "Baotou City 2002 National Economic and Social Development Statistical Bulletin", the annual average temperature in Baotou City in 2002 was 8.5°C, the annual minimum temperature was -27.6°C, the annual maximum temperature was 35.5°C, the annual total precipitation was 262.9 mm, and the annual maximum wind speed was 11.0 meters. / second, the average wind speed is 1.8 meters/second, the annual sunshine hours are 2806 hours, the annual average relative humidity is 52%, and there are 12 sand and dust weather events throughout the year. Summer and autumn are the best seasons in Baotou, with cool breezes, colorful flowers, abundant fruits and vegetables, making it an ideal summer resort.

In winter and spring, the snow is frozen and the snow is covered with snow, which is unique to the North Country