Geographical experts put forward the reasons for the formation of each climate.

Temperate monsoon climate: it appears on the east coast of Eurasia around 35 ~ 55 north latitude, including North China and Northeast China, most of Korea, northern Japan and parts of the Far East of the Soviet Union. In winter, affected by the northerly winds in high latitudes inland, polar continental air masses prevail, which are cold and dry; In summer, influenced by ocean air mass or denatured tropical ocean air mass, southeast wind and southeast wind prevail, which is warm and rainy. Such a climate is called temperate monsoon climate.

Temperate maritime climate: mainly distributed in the west coast of temperate continent, such as the narrow strip of the west coast of Western Europe, North America and South America, with Western Europe as a typical example. Influenced by the prevailing westerly wind all the year round, the ocean airflow blows to the mainland, which is obviously regulated by the ocean. This is called temperate maritime climate.

Temperate continental climate: mainly distributed in the inland areas of Asia-Europe continent and North America continent with latitude of 40 ~ 60. Because it is far away from the ocean and the humid climate is difficult to reach, it is dry and rainy, and the daily temperature difference is greater than the annual temperature difference. Moreover, the closer to the center of the mainland, the drier it is, and the greater the annual and daily temperature difference. More deserts, and so on. This climate is called temperate continental climate.

Tropical rain forest climate: roughly distributed between north and south latitudes 10. Controlled by the equatorial air mass all the year round, it is hot, rainy and humid. The annual average temperature is around 26℃, the annual temperature difference is very small, and the annual precipitation generally exceeds 2000 mm, so the distribution is relatively uniform. This climate is called tropical rain forest climate.

Mediterranean climate: winter is controlled by westerlies, with frequent frontal cyclones and mild climate, with the lowest monthly average temperature of 4 ~ 10℃ and abundant precipitation. Summer is controlled by subtropical high, the airflow sinks, the climate is hot and dry, the clouds are sparse, and the sunshine is sufficient. The annual precipitation is 300 ~ 1000mm, accounting for 60% ~ 70% in winter and only 30% ~ 40% in summer. Climatic characteristics of winter rain and summer drought. The Mediterranean climate is the most special among many climates. It has no fixed position and is concentrated on the Mediterranean coast. This climate is called Mediterranean climate.

Tropical grassland climate: it is distributed between the north and south latitudes 10 and the tropic of cancer, on both sides of the tropical rain forest climate. This area is alternately controlled by equatorial low pressure area and trade wind area. When the equatorial low pressure zone is controlled, the equatorial air mass prevails, forming a humid season, and the weather is sultry and rainy; When the trade winds are controlled, tropical continental air masses prevail, forming a dry season with little rain. This climate is called savanna climate.

Tropical desert climate: it appears in the subtropical high and trade winds on the west coast and inland of the mainland. Controlled by the downward airflow of subtropical high all the year round, there is little precipitation, with the annual precipitation below 250 mm. In some places, it doesn't rain for several years, and the evapotranspiration may be more than 20 times larger than the precipitation. The annual average temperature is higher than 18℃, and it is very hot in summer. The average temperature in the hottest month is mostly 30-35℃, the absolute maximum temperature in some places is as high as 58℃, the maximum temperature on the ground can reach above 80℃, and the average temperature in Leng Yue is not lower than 10℃. The daily temperature difference can reach 35-40℃, and the minimum temperature at night can be reduced to about 0℃. This climate is called tropical desert climate.

Tundra climate: to be precise, it should be called polar climate, which is dominated by polar continental air mass and arctic air mass all year round. The annual average temperature is below 0℃, which is mostly distributed in Eurasia and northern North America. The climate is cold all year round, the temperature in the hottest month is between 0 ~ 10℃, and it is winter all year round. The annual precipitation is below 250 mm, and this climate can only grow tundra communities of lower plants, so it is also called tundra climate.

Not copied. You can't talk about so much climate at once, not too much! ! Hmm. How interesting