A geography problem 1. Compare the differences of climate characteristics among Tokyo, Seoul, Beijing and Ulaanbaatar: 2. Compare the remarkable differences of natural environment in four countries: 3

1 Tokyo has a temperate maritime monsoon climate with four distinct seasons and abundant precipitation. Affected by the southeast monsoon, there is more precipitation in summer. In winter, there is less snowfall.

Seoul has a temperate monsoon climate. The annual average temperature is about 1 1.8℃, with four distinct seasons. There is little rain and warm climate in spring and autumn, which is suitable for traveling. In summer (from June to mid-September), the average monthly temperature is 20℃- 27℃, which is continuous high temperature and rainy weather. In winter (65438+February ~ February), the temperature is slightly lower than other cities in the same latitude. (The monthly average temperature is -5℃~0℃).

Beijing's climate is a typical warm temperate semi-humid continental monsoon climate, with high temperature and rainy summer, cold and dry winter and short spring and autumn.

Ulaanbaatar is a typical continental climate with a large temperature difference in the morning and evening. The lowest temperature in winter can reach -40℃, and the highest temperature in summer can reach 35℃.

Mongolia is a landlocked country in Central Asia, located on the Mongolian Plateau. Mongolia has a typical continental climate. The lowest temperature in winter can reach -40℃, and the highest temperature in summer can reach 35℃.

Central Japan is mountainous and ridged, with hills accounting for 765,438+0% of the total area. Japan is located in the Pacific volcanic earthquake zone, where the Pacific plate collides with the Eurasian plate, with frequent volcanic activity. The latitude of Japan is 25, and the temperature difference between north and south is very significant. The plateaus of Hokkaido and Honshu belong to the sub-frigid zone, the native land belongs to the temperate zone, and the southern islands such as Okinawa belong to the subtropical zone. In addition, Japan's geographical position makes it influenced by the intersection of monsoon and ocean current, so it has four distinct seasons and abundant precipitation.

South Korea belongs to temperate monsoon climate, which has obvious maritime characteristics. Winter is long and cold, summer is hot and humid, and spring and autumn are quite short. The mountainous area accounts for about two-thirds of the area of the Korean peninsula, with diverse topography, low hills and plains interlaced. The plains are mainly distributed in the south and west, and the altitude is mostly below 200 meters.

China's terrain is high in the west and low in the east, showing a ladder shape. Mountains, plateaus and hills account for about 67% of the land area, while basins and plains account for about 33% of the land area. The mountains are mostly east-west and northeast-southwest The continental shelf to the east and south of the coastline is rich in seabed resources.

The climate in China has three characteristics: obvious monsoon characteristics, obvious continental climate and diverse climate types. In winter, the temperature is generally low, hot in the south and cold in the north, and the temperature difference between the north and the south is large, exceeding 50 degrees Celsius.