Quanzhou has a long history and started its economic development as early as the Zhou and Qin Dynasties. In the third year of Wu Yong 'an in the Three Kingdoms (260), Dongan County was established in Fengzhou Town, Nan 'an City. At the end of the Western Jin Dynasty, there was a war in the Central Plains, and a large number of gentry entered the spring.

Quanzhou, also known as Licheng, is a prefecture-level city and a second-class big city under the jurisdiction of Fujian Province. It is one of the central cities in the economic zone on the west side of the Taiwan Strait and a modern industrial and trade port city approved by the Fujian Provincial People's Government. Quanzhou is located in the east of China, east longitude117 25'-19 05', north latitude 24 30'-25 56'. Fuzhou and Putian in the north, Xiamen in the south and Taiwan Province Province in the east. It has subtropical maritime monsoon climate and climatic conditions.

By 2020, the city will have jurisdiction over 4 municipal districts, 3 county-level cities and 5 counties, with a total area of110/5 square kilometers. According to the data of the seventh census, the permanent population of Quanzhou is 8,782,300.

The climate of Quanzhou

Quanzhou is located in low latitude, facing the ocean in the east, and belongs to subtropical maritime monsoon climate, with superior climatic conditions and abundant climatic resources. Quanzhou's climate has three basic characteristics:

First, the temperature is high and the light and heat are rich. The annual total solar radiation is 1.20- 1.40 kcal/cm2, and the annual average temperature in most areas is 1.5-2 1.0℃ (only the northwest mountainous area is lower than 1.8℃). The average temperature in the hottest month is 26-29℃, and it is also 9-0℃ in Leng Yue. The frost-free period is long throughout the year, and the coastal areas are basically frost-free. The effective accumulated temperature ≥ 10℃ is 56 10-7250℃. The annual sunshine hours are 1800-2200 hours.

Second, precipitation is abundant, but it is unevenly distributed in time and space. The annual precipitation of the whole city is 1000- 1800 mm, increasing from southeast to northwest, and the inland area is about twice that of the coastal area. The wet and dry seasons are very clear: the precipitation from March to September accounts for 80% of the whole year, which is the rainy season; 10-February only accounts for 20% of the whole year, belonging to the dry season. The interannual variation rate of precipitation is large, and the precipitation in less rainy years is less than half of that in rainy years.

Third, the monsoon climate is remarkable. The winter half year is mainly controlled by Mongolian cold high pressure wedge, with prevailing northerly wind, low temperature and little rain; Summer is mainly affected by subtropical high, prevailing southerly wind, high temperature, humidity and rain.

Reference to the above content: Baidu Encyclopedia-Quanzhou City