Climatic characteristics of high temperature in summer

In summer and solar terms, the temperature begins to drop. The direct point of the sun continued to move southward, the solar radiation weakened, the western Pacific subtropical high retreated southward, and the Mongolian cold high began to itch to try. Under the control of cold and high pressure, sinking dry cold air is formed, and the rainy season in Northeast China, North China and Northwest China ends, taking the lead in starting the best weather in a year-crisp autumn.

Being in summer is the fourteenth of the twenty-four solar terms. Dou refers to Wu (southwest), and the yellow meridian of the sun reaches 150, which is celebrated on August 22-24 of the Gregorian calendar every year. Being in the heat is "out of the heat", that is, out of the heat. In summer, the direct point of the sun continues to move southward, the solar radiation weakens, the subtropical high also withdraws southward, the temperature gradually drops, and the summer heat gradually disappears.

Introduction:

The weather in summer is generally around 30℃, subject to the local real-time weather forecast. The temperature in summer is generally about 65438 0.5℃ lower than that in early autumn, and it fluctuates around 30℃ in most parts of China. The arrival of the summer heat marks the end of the hot weather, and the summer heat gradually fades, from hot to cold. It is not enough to describe the summer solar terms simply by the beginning of low temperature, and the low temperature is only one of the phenomena.