Which dry, wet and warm zone does Inner Mongolia Plateau belong to?

The eastern part of Inner Mongolia Plateau is semi-arid and the western part is arid. Temperature zone: middle temperate zone.

The altitude of Inner Mongolia Plateau is generally 1000 ~ 1200m, which is high in the south and low in the north. East-west lowlands are formed in the north, and the lowest elevation drops to about 600 meters. The topography of Inner Mongolia Autonomous Region is dominated by plateau, which is complex and diverse.

Hulunbeier Plateau, Xilingol Plateau, Wulanchabu Plateau, Bayannaoer-Alashan Plateau and Ordos Plateau in southern Inner Mongolia are called the five major plateaus. The ground is flat and endless.

Climate of Inner Mongolia Plateau

The Inner Mongolia Plateau is far away from the ocean and mountains are separated, and the climate is dominated by temperate continental monsoon climate. The precipitation is small and uneven, and the wind is strong. Summer is short and hot, precipitation is concentrated, autumn temperature drops suddenly, frost often comes early, winter is long and cold, and there are many cold waves The east of Helan Mountain is a semi-arid area, and the west of Helan Mountain is an arid area, belonging to the middle temperate zone, and the precipitation decreases from east to west.

Inner Mongolia Plateau has weak summer monsoon, strong winter wind (close to the winter wind source), dry climate, cold winter and abundant sunshine (clear weather and strong evaporation). The annual average temperature is 3 ~ 6℃, which is high in the west and low in the east.

The distribution of annual precipitation in Inner Mongolia Plateau is less in the east and less in the west (precipitation is pushed inland from the ocean), and the annual variation rate of precipitation is large.