Climatic types in northern China

The northern region belongs to temperate monsoon climate. The areas north of Qinling-Huaihe Line, Daxing 'anling and Wushaoling East include all or most of the t

The northern region belongs to temperate monsoon climate. The areas north of Qinling-Huaihe Line, Daxing 'anling and Wushaoling East include all or most of the three northeastern provinces, five provinces and two cities in the middle and lower reaches of the Yellow River, southeastern Gansu, eastern and northern Inner Mongolia, Jiangsu and northern Anhui. The terrain is mainly plain, with both plateau and mountain, and is rich in grain and mineral resources.

The northern region includes Beijing, Tianjin, Hebei, Shanxi, Shaanxi, Gansu, Henan, northern Jiangsu, Shandong, northern Anhui, Heilongjiang, Jilin, Liaoning and Inner Mongolia. It is one of the four geographical divisions of China, which refers to the vast areas north of Qinling Mountains and Huaihe River, south of Inner Mongolia Plateau, east of Daxinganling Mountains and Qinghai-Tibet Plateau, and east of Bohai Sea and Yellow Sea, mainly including Guanzhong area, kanto region, North China and Northeast China.

The northern region is mainly temperate continental climate and temperate monsoon climate. It is lower than 0℃ in winter and higher than 20℃ in summer, and the temperature changes obviously in four seasons. The most Leng Yue appeared in 65438+ 10 month, and the hottest month was in July. The annual precipitation is small, the seasonal distribution is uneven, and the precipitation is concentrated in summer.

The temperate monsoon climate is distributed on the east coast of the mid-latitude continent in the northern hemisphere, with an annual average temperature of not less than 0℃ and an annual accumulated temperature of 3200℃-4500℃. Summer is hot and rainy, winter is cold and dry, and the four seasons are distinct, which belongs to the transitional climate between subtropical and temperate zones.