Chaozhou has a subtropical maritime monsoon climate with long summer and short winter, abundant sunshine, mild climate and abundant rainfall. There is no snow all year round, with an annual average temperature of 265,438 0.4℃, an extreme maximum temperature of 39.6℃ and an extreme minimum temperature of -0.5℃. The average annual rainfall is 1685.8 mm, which is a natural incubator.
In winter (12 ~ February), northeast wind or north wind prevails. After a long journey, the dry and cold air from the north was warmed and wet, and its intensity was greatly weakened. In Guangdong, the wind speed has become smaller and the temperature is higher, so Chaozhou is warmer in winter. However, when the cold wave comes, frost weather will also occur in individual years.
Winter is the dry season in Chaozhou, with less precipitation, sunny weather and plenty of sunshine. The month of 65438+ 10 is the most Leng Yue, the monthly average temperature is 9 ~ 16℃, and the temperature difference between north and south is above 7℃. The extreme minimum temperature has been recorded at MINUS 7.3℃, and the extreme minimum temperature in Chaozhou for many years is 0℃.
In Chaozhou, although winter is influenced by the cold air in the south, due to the low latitude, the average temperature in 65438+ 10 is still 13.5℃, so there is no winter in the climate sense.
Chaoshan geographical environment
Chaoshan area is located in the east of Guangdong Province, and Rongjiang River flows through the lower reaches of the Han River from north to south, dividing Chaoshan area into north and south parts. From Fenghuang Mountain in Fengshun County in the north to Lei Ling in Huilai County in the south, its watershed constitutes the geographical dividing line of Chaoshan Plain.
It mainly includes Shantou, Jieyang and Chaozhou. Although Shanwei is not in the Chaoshan plain, its language and culture are similar to those in Chaoshan area, so Shanwei is often regarded as a part of Chaoshan area.
Chaoshan area is located in the land-sea interaction zone, with high terrain in the northwest and low terrain in the southeast, showing a stepped decline. The landform types are mainly mountains and hills, followed by platforms and plains.
Hanjiang River is the mother river in Chaoshan area. The Hanjiang River, which originated in the northern mountainous area of Chao 'an, flows through the whole Chaoshan area from west to southeast, dividing the Chaoshan area into north and south parts. The mountains in the north are steep and steep, and the hills in the south are mainly gentle slopes.
Reference to the above content: Baidu Encyclopedia-Chaoshan