What is the main climate type in Beijing?

The climate type in Beijing is mainly temperate monsoon climate.

The climate type in Beijing is mainly temperate monsoon climate, with obvious seasonal changes. In winter, influenced by Mongolian high pressure, northwest wind prevails and the climate is cold and dry; In summer, influenced by the Pacific subtropical high, the southeast wind prevails, and the climate is warm, hot and humid. In spring (March-May), the temperature gradually rises and the weather gets warmer. However, due to the frequent cold air activities, the temperature fluctuates greatly, and sometimes there will be cold waves, strong winds, frost and other weather.

In summer (June-August), the temperature is high, the humidity is high, the precipitation is concentrated, and sometimes there will be heavy rain, lightning, hail and other weather. Summer is also the rainy season in Beijing, and the average precipitation accounts for more than 60% of the whole year. In autumn (September to165438+1October), the temperature is gradually decreasing, the weather is clear and the autumn air is crisp, which is the season for tourism and harvest. In winter (65438+February to February), the temperature is low and the weather is cold, and sometimes there will be heavy snow, freezing rain and other weather. Winter is the coldest season in Beijing and also the heating period.

Generally speaking, the climate in Beijing is characterized by four distinct seasons and large temperature difference. Due to the change of climate, rich natural and cultural landscapes have also been formed, attracting a large number of tourists to visit. At the same time, climate change has also had an important impact on agriculture, transportation and urban planning in Beijing.

Introduction to climate types:

1, tropical rain forest climate, characterized by high temperature and rainy all year round, and even precipitation distribution; Distribution: mainly within 5 north and south latitudes; Reason: It is controlled by equatorial low all the year round.

2. Tropical grassland climate, characterized by high temperature all year round, divided into obvious dry season and rainy season; Distribution: Latitude 5-10; Cause of formation: subtropical high and equatorial low are alternately controlled.

3. Tropical monsoon climate, characterized by high temperature all year round and obvious dry and wet seasons; Distribution: Southeast Asia and South Asia; Reason: Controlled by southwest monsoon.

4. Tropical desert climate, characterized by high temperature and drought all the year round; Distribution: the mainland near the Tropic of Cancer or the west coast of the mainland; Reason: It is controlled by subtropical high all the year round.

5. Subtropical monsoon climate, characterized by high temperature and rainy in summer and low temperature and little rain in winter; Distribution: 25-35 degrees north latitude, east coast of mainland China; Cause of formation: alternating control of winter and summer monsoon.

6. Mediterranean climate, characterized by hot and dry summer and mild and rainy winter; Distribution: 30-40 degrees north latitude, west coast of mainland China; Cause of formation: alternating control of wind belt and subtropical high.

7. Temperate monsoon climate, characterized by high temperature and rainy summer and cold and dry winter; Distribution: Northeast Asia; Cause of formation: alternating control of winter and summer monsoon.

8. temperate continental climate, characterized by large annual temperature difference and scarce precipitation; Distribution: Mid-latitude inland; Reason: It is controlled by continental air mass all the year round.

9, temperate maritime climate, characterized by mild and humid, uniform precipitation; Distribution: 40-60 continental west coast; Reason: it is controlled by the west wind all the year round.

10, the climate characteristics of coniferous forest in sub-cold zone are long and cold in winter and short and cool in summer; Distribution: the continental latitude is higher; Genesis: high latitude, controlled by sub-polar depression.