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广州气候资料(Climatological information for guangzhou)
广州气候资料(Climatological information for guangzhou)
Guangzhou climate source: guangdong meteorological network
Source: liu bizhus diary
Guangzhou is located in the tropical monsoon climate zone of South Asia, the climate is characterized by high temperature, more precipitation, less frost, more sunshine, less wind speed and more thunderstorm.
High temperature, annual average temperature 21.9 ℃. Years, with the highest average temperature in July, 28.4 ℃. In January, while the temperature is low, but the monthly mean temperature is still in 13 ℃ above. The temperature of the poor 15 ℃. Therefore, it can be said that the temperature is high all year round. For many years, the extreme maximum temperature 39.1 ℃, appeared in the July 1, 2004). The highest temperature 30 ℃ or more heat, since July 11 to August 20, an average of 41 days. Over the years, extreme minimum temperature of 0 ℃ (appeared in the February 11, 1957), the year of more than 80% of the minimum temperature in more than 1 ℃. In recent years, the longest winter has been 21 days, showing up on December 26, 1976, and January 15, 1977, and January 21, 1984.
Precipitation is more -- the annual average precipitation is 1696.5 mm. Of course, there is a big difference between annual and annual precipitation. In 1975, the annual precipitation reached 2516.7 mm, while in 1956 it was only 1158.0 mm, which is more than twice the difference. However, the annual precipitation in most years is above 1380mm. The average rainfall in the four to September months of the year was more than 150mm, and in May and August more than 220mm, including 288.7 mm in May. During the dry season from October to march, the average precipitation in each month was not too small, with 40 to 60 mm, even in December, when the precipitation was the lowest, and the average monthly precipitation was 24mm. The average annual rainstorm day is 63 days, and the main concentration appears in the five to September period, with an average of one day in e
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