What's the difference between the weather in Fujian and that in Beijing?

Fujian is located in the southeast of the motherland, on the coast of the East China Sea. It belongs to subtropical humid monsoon climate. There are mountains in the northwest to block the cold wind, and the southeast is regulated by the sea breeze. A warm and humid climate is a remarkable feature of the climate. Taking Fuzhou-Fuqing-Yongchun-Zhangping-Shanghang as the boundary, it can be divided into middle subtropical zone and south subtropical zone. Its main features are as follows: First, the monsoon climate is remarkable. The cold and warm climate, the beginning and end of the four seasons, all shift with the activity of monsoon circulation. Second, winter is short and summer is long, with abundant heat resources. Third, the winter is warm, and the temperature difference between north and south is large; It is cool in summer, and the temperature difference between north and south is small. Fourth, the rainy season and dry season are distinct, and water resources are abundant. Fifth, complex terrain leads to diverse climate. The six-year average temperature 15℃-22℃ rises from northwest to southeast. 1 month 5℃- 13℃, July 25℃-30℃. The extreme minimum temperature is -9.5℃. The extreme maximum temperature is 43.2℃. The frost-free period is 240-330 days, and there is almost no frost to the south of Mulan River. The average annual precipitation is 800- 1900 mm, which is less in coastal areas and islands, and more in mountainous areas in northwest China. On September 1963, the precipitation in Mazu was 380mm, which was the highest daily precipitation recorded in this province. The rainfall is the highest from May to June every year, and there are many typhoons and rainstorms at the turn of summer and autumn.