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Climates are classified based on specific criteria unique to each climate type. [1] The Köppen climate classification is the most widely used climate classification scheme. [2] It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [3] [4] with several later modifications by Köppen, notably in 1918 and ...
A tropical rainforest climate or equatorial climate is a tropical climate sub-type usually found within 10 to 15 degrees latitude of the equator. There are some other areas at higher latitudes, such as the coast of southeast Florida, United States, and Okinawa, Japan that fall into the tropical rainforest climate category.
Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. The most used is the Köppen climate classification scheme first developed in 1884. [1] [2]
Tropical rainforest climate#Equatorial climates and tropical trade-wind climates From a page move : This is a redirect from a page that has been moved (renamed). This page was kept as a redirect to avoid breaking links, both internal and external, that may have been made to the old page name.
The climate of Ecuador is generally tropical and varies with altitude and region, due to differences in elevation and, to a degree, in proximity to the equator. [ 1 ] [ 2 ] Ecuador map of Köppen climate classification.
The climate of Cameroon is very diverse. Cameroon is generally referred to as the Africa in miniature because it has the major climates and vegetation of the continent. The country is separated in two main climatic zones: the equatorial climate in the south and the tropical climate in the northern part. [1]
The ITCZ is visible as a band of clouds encircling Earth near the Equator. The Intertropical Convergence Zone (ITCZ / ɪ tʃ / ITCH, or ICZ), [1] known by sailors as the doldrums [2] or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge.
[1] Still another definition states that the thermal equator is the latitude at which insolation is identical throughout the year. This is not the same as the astronomical equator because Earth reaches perihelion (the minimum distance from the Sun in its orbit) in early January and is at aphelion (maximum distance) in early July. Therefore ...