What's the climate like in 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. The climate in Quanzhou has three basic characteristics: First, the temperature is high and the light and heat are sufficient. Annual total solar radiation 1.20- 1.40 kcal/cm2, annual average temperature 1.5-2 1.0℃ in most areas, average temperature in the hottest month is 26-29℃, and average temperature in Leng Yue is 9-/kloc-0.

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.

Topography of Quanzhou city

Quanzhou geotectonics is located in the southeast of South China fold system, and in the south-central part of eastern Fujian volcanic rift zone. The structural belts are all distributed in northeast-southwest direction. More than four-fifths of the country is distributed in Mesozoic volcanic rocks and intrusive rocks, accounting for about half of the exposed area, and the distribution area of intrusive rocks increases from northwest to southeast to become the main body.

The trunk of Daiyun Mountain in the middle of Fujian-Zhongshan system is distributed in northeast-southwest direction, located in Dehua in the northwest, with a huge scale. The elevation of the main peak is1856m, which is the second highest peak in Fujian province. Its branches and residual veins extend to the southeast and south, and the terrain is high in the northwest, and gradually decreases to the southeast, forming a multi-layer landform landscape that gradually changes from low-middle mountains to hills and platforms to plains.

Reference to the above content: Baidu Encyclopedia-Quanzhou City