Climate differences between Britain and Foshan

According to Baidu Library, the climate difference between Britain and Foshan is mainly reflected in the following aspects:

1. Humidity: The climate in Britain and Guangdong is humid, but the degree and manifestation of humidity are slightly different. In Britain, due to the influence of the Atlantic maritime climate, most of the year is humid, and high humidity makes the air feel humid. Guangdong is located in the subtropical monsoon climate zone, which is characterized by the same season of rain and heat, wet and cold spring, long summer without heat, warm and sunny autumn and winter. So the air humidity is high, which makes people feel wet.

2. Precipitation and sunshine: In Britain, there is a lot of rainfall and little sunshine, which makes the western part of Britain unsuitable for the growth of food crops, but juicy pastures grow well, thus promoting the development of dairy industry. In the southeast of England, there is less precipitation, more sunshine, high temperature and long growing period, which is beneficial to agricultural production. The average annual precipitation in Foshan is between 1620 ~ 1690 mm, and the distribution is uneven. The rainy season is concentrated from April to September, accounting for about 80% of the annual precipitation. The spatial and temporal distribution of precipitation in summer is uneven, and the rainfall in autumn and winter is obviously reduced. The annual average sunshine hours are more in the south and less in the north. Spring is rainy and rainy, which is the season with the least sunshine.

3. Temperature: It is mild in Britain and cool in Leng Xia in winter. Guangdong has a hot and humid climate, with long and hot summers and short and warm winters.