What are the climatic characteristics of China in spring?

Spring is the period when the weather changes the most in a year, when the temperature changes from warm to cold and suddenly changes. The temperature difference in a day is the largest in spring. Taking Beijing as an example, the difference between the highest temperature and the lowest temperature reached 26.8℃ on May 3rd, 1966.

2. The air is dry and windy

Spring is the transitional season between winter and summer, and the cold and warm air are equally strong, both of which are very active, so windy weather often occurs, especially in northern China, which is characterized by alternating north-south winds and strong winds. Generally speaking, the phenomenon of frequent north-south winds can be improved after May.

3. Dust weather in the north

In spring, with the temperature rising, if there is little precipitation, the ground is dry and the wind comes, it is easy to have dusty weather. Meteorology, sandstorm weather is divided into floating dust, sand blowing and sandstorm. In northern China, March and April are the frequent periods of dusty weather.

It is rainy in the south.

In early spring or late autumn in China, it rained continuously for several days or even months, and the weather was cold and there was almost no sunshine. Also known as low temperature and continuous rain. It is often rainy and rainy in southern spring, with low temperature and warm temperature appearing alternately. Humidity in rainy season is high, which is easy to cause rheumatoid arthritis. In addition, it also has a great influence on people's psychological diseases. Therefore, special attention should be paid to adapting to nature and climate change in spring.

Influencing factors of climate in China;

1, latitude factor: the temperature in China gradually decreases from south to north. (Scope of influence: the whole country)

2. Land and sea factors: China lies between Asia and Europe, the largest continent in the world, and the largest ocean and Pacific Ocean in the world.

The huge thermal difference between land and sea forms a typical monsoon climate, that is, the south wind blows in summer and the north wind blows in winter.

3. Topographic factors: The higher the altitude, the lower the temperature. On high mountains, the climate changes vertically. (Scope of influence: Qinghai-Tibet Plateau is the most significant. )