What are the characteristics of subtropical monsoon humid climate?

1. The subtropical monsoon climate is distributed on the east coast of subtropical continent at 25 ~ 35 north latitude, which is due to the alternate control and competition between tropical marine air mass and polar continental air mass. It is mainly distributed in the south of Huaihe River in Qinling Mountains in eastern China, north of tropical monsoon climate, south of Japan and south of Korean Peninsula. It's not cold here in winter. The average temperature in 65438+ 10 is generally above 0℃, and it is hot in summer. The average temperature in July is generally around 25℃, and the direction of Xia Feng changes obviously in winter. The annual precipitation is generally above 1000 mm, mainly concentrated in summer and less in winter. This climate is most typical in the southeast of China. In other areas, because there is a considerable amount of precipitation in winter, there is little difference between winter and summer, so it is called subtropical monsoon humid climate. In fact, subtropical monsoon climate = subtropical monsoon humid climate, but the statement is different.

2. The subtropical monsoon climate is humid, with abundant sunshine and rainfall. There is no snow and little frost all year round. The annual average temperature is 2 1.4℃, the annual total solar radiation 1 15- 156 kcal per square centimeter, and the annual average precipitation1720-.

Thirdly, the subtropical monsoon climate is more obvious than the subtropical monsoon humid climate, because the difference between land and sea is greater, so the seasonal variation of precipitation and temperature is greater than that of the subtropical monsoon humid climate.