This however, is followed by a sustained period of high rainfall for two or more consecutive months. extraordinarily rainy wet seasons and pronounced dry seasons - pronounced dry seasons similar in length and character to dry seasons observed in tropical savanna climates.less pronounced dry seasons - substantial amount of rain during the wet season, usually in the form of frequent thunderstorms, however considerable amount also falls during the dry season.There are generally two versions of this climate type: The dry period is usually much shorter than the wet one. Temperatures are high all year and precipitation can be lower during some months, overall however, the total annual precipitation is often greater than that of equatorial climate (Af), where it is just more evenly distributed. For example in Asia during the summer, wind blows from the ocean to land, in the winter it is the other way around. These are seasonal winds changing direction during the year. Most significant factor that determines the climate are the monsoons. This type of climate is most often encountered in South and Central America, some parts of South and Southeastern Asia, western and central part of Africa, the Caribbean and parts of North America. The temperature range during the day remains more less constant throughout the year and the driest month usually is the one right after or close to the winter solstice in that particular hemisphere. Tropical monsoon climate is characterized by alternating dry and wet periods, similar to the tropical climate of savannas. m – precipitation of driest month less than 60mm (2.35in), but greater than or equal to 100-0.04r (where r is the total average precipitation in mm).Tropical microclimate, however, is also found in some other regions such as for example the northern part of Queensland in Australia or the eastern part of Madagascar. This climate is quite common in Southeast Asia, central Africa and South America. Therefore common plant species include many types of ferns and mosses, as well as epiphytes (plants growing harmlessly upon another plant). The tree canopy often shields most of the sun light and only a fraction reaches the smaller plants near the forest floor. Main vegetation of this climate is trees, which can be over 50 m (165 ft) high. The climate is very humid because of the rainfall, which is often above 2500 mm/year (100 in) and there is no dry season. Also thunderstorms are quite common and most intense rains usually occur late in the afternoon and in the evening. The average temperature during the day remains high all year round, quite often above 30☌ (85☏). Differences between temperatures during day and night can be significant. The temperature and precipitation distribution remains more less the same throughout the year and the same also applies for the duration of day and night, which remains constant due to the position near the equator. There are also no seasons during the year. The climate is characterized by an absence of a dry period, all months having precipitation amount of at least 60 mm (2.35 in). It is usually areas covered with tropical rainforests. This type of climate, sometimes also called equatorial climate, is typical for regions close to the equator, most often 5 to 10 degrees south or north from it. f – precipitation of all months at least 60 mm (2.35 in).A – average temperature of coldest month higher than 18☌ (65☏).Tropical rainforest climate (Equatorial climate)
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