What's the temperature in Anhui in winter?

The average temperature in Anhui Province is between-1 ~ 4℃ in winter, around 28 ~ 29℃ in summer and July, and it is below 30℃ all over the year, so the continental climate is not obvious. Except for a few years, the cold and hot periods are generally short.

The annual precipitation in Anhui province is between 750- 1700 mm, showing the characteristics of more in the south and less in the north, more in the mountains and less in the plains and hills. Huaibei is generally below 900 mm, Jiangnan, western Jiangnan and Dabie Mountain are above 1200 mm, and the rainfall lines such as 1000 mm run through the middle of Jianghuai hilly area. Precipitation in mountainous areas generally increases with height, and the average annual rainfall in Guangmingding of Huangshan Mountain reaches 2300 mm.

According to the national precipitation distribution map, the rainfall in Anhui Province is moderate, which can meet the needs of crop growth and development in general years.

May is the transition period between winter wind direction and summer monsoon. The north-south airflow competes with each other, advancing and retreating freely, the front belt moves north and south, the cyclone activity is frequent, and the weather and climate are changeable. So it is a major feature of the spring climate in our province. The temperature rise in spring is unstable and changes greatly every day. The temperature in spring is lower than that in autumn, and the spring rain is more than the autumn rain.

Rainwater problem in Anhui;

The precipitation in March, April and May accounts for about 20-38% of the annual precipitation, increasing from north to south. The rainy season in the south of the Yangtze River comes early, and the annual rainfall concentration period is in April, May and June. Spring rain is more than summer rain in Jiangxi, Tunxi and Qimen. In spring, the low temperature and abundant spring rains, especially the long-term low temperature and continuous rain, are unfavorable to the seedling growth of spring-sown crops such as early rice and cotton.

In autumn, in addition to the cold high pressure on the ground, the subtropical warm high pressure is still maintained at high altitude, and the atmospheric stratification is relatively stable. The autumn is crisp and sunny.