What is the climate like in Kyoto?

Beijing is located in the northern part of the North China Plain, backed by Yanshan Mountain, and adjacent to Tianjin City and Hebei Province. Beijing's climate is a typical north temperate zone semi-humid continental monsoon climate.

Beijing has a continental monsoon climate, with hot and rainy summers and cold and dry winters. The average annual temperature is 10 to 12 degrees Celsius. The temperature is minus 7 to 4 degrees Celsius in January and 25 to 26 degrees Celsius in July. The extreme minimum is minus 27 degrees Celsius, and the extreme maximum is above 42 degrees Celsius. The frost-free period lasts 180 to 200 days throughout the year, and is shorter in the western mountainous areas. The average annual rainfall is more than 600 mm, making it one of the areas with the highest rainfall in North China. The windward slope of the mountain front can reach more than 700 mm. The seasonal distribution of precipitation is very uneven. The precipitation throughout the year is concentrated in the three months of June, July and August in summer, and there are often heavy rains in July and August.

Continental monsoon climate is one of the most basic climate types on the earth. Its general characteristic is that it is greatly affected by the continent and less affected by the ocean. Under continental climate conditions, both solar radiation and ground radiation are large. Therefore, the temperature in summer is very high, the air pressure is very low, it is very hot, and the humidity is high. In winter, controlled by cold and high pressure, the temperature is very low and very dry.