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热带地区的主要气候类型有(The main types of climate in the tropics are)
热带地区的主要气候类型有(The main types of climate in the tropics are) The main types of climate in tropical regions: (1) tropical rain forest climate (also called equatorial rainforest climate). Located on both sides of the equator of the continent, South and North stretches 5 degrees to about 10 degrees, such as the Amazon plain in South America, the Congo basin in Africa and the Gulf coast of Guinea, and some islands in Southeast asia. The area is located in the equatorial low, air upward motion, water vapor condensation caused by the chance of rain, rainy year, no dry season, annual rainfall of 2000 mm or more, at least the pluv precipitation is more than 60 mm, and more thunderstorms; the mean temperature of 25 DEG to 28 DEG C, the long summer, no the seasonal variation range, generally less than 3 degrees, while the average daily range can reach 6 DEG to 12 DEG C. Under the climate of high temperature and rain all the year round, plants can grow year by year, with many kinds of trees and dense vegetation. (2) tropical wet and dry season climate (also known as the tropical steppe climate). This climate is mainly distributed on both sides of the equatorial rainy climate zone, namely, South and north latitude 5 degrees to about 15 degrees (some reach 25 degrees) in Central America, South America and africa. The main characteristics, first is due to the influence of equatorial low wind zone and North-South movement, alternately, a year of dry and wet season. When the equatorial belt of low pressure control, the prevalence of the equatorial ocean air masses, and there is convergence updraft formed in wet season, humid and rainy, with dense growth over the high grass and shrubs, and miscellaneous trees, namely the savanna landscape. When affected by the trade winds, the prevalence of tropical continental air, dry and little rain, the formation of the dry season, soil dry, yellow grass, deciduous trees. Compared with the equatorial climate, a year at least 1 to 2 months of th
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