What are the climate characteristics of the 12 climate types?

1. The basic characteristics of the distribution patterns, characteristics and distribution patterns of the world's major climate types. The main causes are tropical rain forest climates. Low pressure areas on both sides of the equator are controlled by low pressure all year round, with no obvious seasonal changes. They are affected by equatorial low pressure all year round. Controlled, multi-convective rain savanna climate tropical rainforest climate The trade wind belts on the north and south sides have high temperatures all year round, with obvious dry and wet seasons (precipitation is about 1000 mm). The trade wind belts and equatorial pressure zones alternately control the tropical monsoon climate Northeast China The southern and southeastern parts of the continent within the wind belt have high temperatures all year round, with obvious rain and dry seasons (precipitation is about 2000 mm). The thermal difference between sea and land and the seasonal movement of the air pressure belt in the wind belt. Tropical deserts. The west coast of the continent near the Tropic of Cancer and the interior of the continent are hot and dry all year round. Controlled by the subtropical high pressure belt and trade wind belt, the subtropical monsoon and monsoon humid climate is 30°-40° north and south latitude. The east coast of the continent is hot and rainy in summer, and the winter is mild and less rainy. The thermal difference between sea and land is Mediterranean climate. The summer is hot and dry on the west coast of the continent at 30°-40° north and south latitude. , mild and rainy winters, subtropical high pressure belts and westerly belts alternately control temperate oceanic climate, 40°-60° north and south latitude, the west coast of the continent has mild winters, cool summers, uniform precipitation throughout the year, controlled by westerly belts all year round, temperate continental climate, temperate continental interior, cold winters and summers Hot, with large annual variations, precipitation is sparse and concentrated in summer, far away from the ocean, and moist airflow is difficult to reach. Temperate monsoon climate. Northeastern Asia is hot and rainy in summer, and cold and dry in winter. The thermal difference between sea and land is polar climate. The North and South Poles are cold all year round, with scarce precipitation. High latitudes, receiving sunlight Less light and heat. Generally speaking, the climate types on the west coast of the mainland are mainly controlled by pressure and wind belts. Students should distinguish between climate types controlled by a single pressure and wind belt, and climate types controlled by alternating pressure and wind belts. The east coast of the continent is mainly controlled by monsoon circulation.