What climate type does Suzhou and Hangzhou belong to? What is the difference between Beijing and Beijing?

Suzhou and Hangzhou belong to subtropical monsoon climate, with high temperature and rainy summer and mild and little rain in winter. Beijing has a temperate monsoon climate, which is hot and rainy in summer and cold and dry in winter. There is a lot of precipitation in Suzhou and Hangzhou, and the temperature in winter is above 0 degrees; There is little precipitation in temperate monsoon climate, and the temperature in winter is below 0 degrees.

I. Subtropical monsoon climate

The subtropical monsoon climate is mainly distributed on the east coast of subtropical continent with latitude of 22 ~ 35. It is a zone where tropical marine air masses and polar continental air masses alternately control and compete with each other. It is mainly distributed in the south of Huaihe River in Qinling Mountains in eastern China, the north of Leizhou Peninsula, the south of Japan and the south of Korean Peninsula. In addition, China, Hainan and Taiwan Province provinces have subtropical monsoon climate. This is a unique climate in Asia.

The climate zone is not cold in winter, and the average temperature in June is generally above 0℃ at 5438+ 10, and it is hot in summer, and the average temperature in July and August is generally around 25℃-35℃. Due to the influence of ocean airflow, the annual precipitation is generally above 800 ~ 1000mm, which belongs to humid areas.

Second, the temperate monsoon climate

The temperate monsoon climate lies between Eurasia, the largest continent, and the Pacific Ocean, and the thermal properties of land and ocean are significantly different. In summer, the Eurasian continental depression is connected, the ocean subtropical high extends westward and advances northward, and the southeast monsoon from the subtropical high in the North Pacific brings abundant precipitation. The northwest monsoon from the powerful Mongolian high in winter affects the local area. Because the wind shear meets the requirements of monsoon, it is a monsoon climate.

In winter, affected by the northerly winds in high latitudes inland, polar continental air masses prevail, which are cold and dry; In summer, influenced by polar ocean air mass or denatured tropical ocean air mass, southeast wind and southeast wind prevail, with warm, hot and rainy seasons. The annual precipitation is mostly 500~ 1000mm, of which about 2/3 is concentrated in summer (hot and rainy in summer and cold and dry in winter). There are four distinct seasons throughout the year and the weather is changeable. With the increase of latitude, the temperature amplitude in winter and summer increases correspondingly, while the precipitation decreases gradually.