Traditional Culture Encyclopedia - Weather inquiry - How is the high temperature weather in Baotou formed?

How is the high temperature weather in Baotou formed?

1, located in temperate continental climate, with less precipitation and large evaporation, which aggravated the high temperature;

2. Living deep inland, cut off by mountains (Taihang Mountain, etc.). ), moist air from the ocean arrives less, sunny days are more, and the temperature is high;

3. Close to Kubuqi Desert, the vegetation coverage rate is low, the specific heat capacity is low, and the temperature is high in summer.

However, because Baotou is located at the southern foot of the yinshan mountains, with an average elevation above 1000m, and can be slightly affected by the warm and humid air flow from the Pacific Ocean, the temperature is not too high compared with that in the same latitude, and the average temperature in July in the hottest month is lower than that in Beijing in the same latitude.

Baotou has a long and cold winter, little rain and snow, dry and windy spring, short-term concentrated hot rain in summer, crisp autumn and early frost. Baotou City is located at the southern tip of Mongolian Plateau, with the Yellow River in the south and the yinshan mountains running through the middle of the city. There are Tumochuan Plain and Hetao Plain on the east and west sides, which are located at 4015' to 4129' north latitude, 0/09 22' east longitude and 0/0/0 07' east longitude respectively. It is1067.2m above sea level, far away from the ocean, living inland, and belongs to semi-arid mid-temperate continental monsoon climate. The scenery here is pleasant and the temperature is moderate, with an average annual temperature of 7.2℃.