Information about Tropical Climate

Climate is the average and variations of weather over long periods of time. Climate zones can be defined using parameters such as temperature and rainfall.
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tropics are the geographic region of the Earth centered on the equator and limited in latitude by the Tropic of Cancer in the northern hemisphere, at approximately 23°30' (23.5°) N latitude, and the Tropic of Capricorn in the southern hemisphere at 23°30' (23.5°) S latitude.
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Wladimir Köppen

1921, photo by Friedrich Becks
Born September 25, 1846
Saint Petersburg, Russia
Died June 22, 1940
Graz, Austria
Nationality Russian/German
Ethnicity German
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Köppen climate classification is one of the most widely used climate classification systems. It was developed by Wladimir Köppen, a German climatologist, around 1900 (with several further modifications by Köppen himself, notably in 1918 and 1936).
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In general terms, the climate of a locale or region is said to be arid when it is characterized by a severe lack of available water, to the extent of hindering or even preventing the growth and development of plant and animal life.
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Climate is the average and variations of weather over long periods of time. Climate zones can be defined using parameters such as temperature and rainfall.
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equatorial climate is a type of tropical climate in which there is no dry season – all months have mean precipitation values of at least 60mm. It is usually found at latitudes within five degrees of the equator – which are dominated by the Intertropical Convergence Zone.
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monsoon is a seasonal prevailing wind which lasts for several weeks with no lasting climatic effects. The term includes almost all of the phenomena associated with the annual weather cycle within the tropical and subtropical land regions of the earth.
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savanna or savannah is a tropical or subtropical woodland ecosystem. Savannas are characterised by the trees being sufficiently small or widely spaced so that the canopy does not close.
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In general terms, the climate of a locale or region is said to be arid when it is characterized by a severe lack of available water, to the extent of hindering or even preventing the growth and development of plant and animal life.
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A Semi-arid climate or steppe climate generally describes climatic regions that receive low annual rainfall (250-500 mm or 10-20 in). A more precise definition is given by the Köppen climate classification that treats steppe climates (BS) as intermediates between the desert
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The humid subtropical climate (Köppen Cfa) is a climate zone characterized by hot, humid summers and chilly to mild winters. This climate type covers a broad category of climates, and the term "subtropical" may be a misnomer for the winter climate in the cooler areas within this
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oceanic climate (also called marine west coast climate and maritime climate) is the climate typically found along the west coasts at the middle latitudes of all the world's continents, and in southeastern Australia.
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Mediterranean climate is a climate that resembles the climate of the lands in the Mediterranean Basin. Outside the Mediterranean, this climate covers relatively small areas of the Earth, and generally occurs on the western coasts of continental landmasses, roughly between
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The humid continental climate is a climate found over large areas of land masses in the temperate regions of the mid-latitudes where there is a zone of conflict between polar and tropical air masses.
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Regions having a subarctic climate (also called boreal climate) are characterized by long, usually very cold winters, and brief, warm summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N.
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Mediterranean climate is a climate that resembles the climate of the lands in the Mediterranean Basin. Outside the Mediterranean, this climate covers relatively small areas of the Earth, and generally occurs on the western coasts of continental landmasses, roughly between
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polar climate are characterized by a lack of warm summers (specifically, no month having an average temperature of 10 °C or higher).

Types of polar climate

There are two distinct types of polar climate.
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Alpine climate is the average weather (climate) for a region above the tree line. The climate becomes colder at high elevations—this characteristic is described by the lapse rate of air: air will tend to get colder as it rises, since it expands.
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