Tropical savanna climate

Worldwide zones of Tropical savanna climate (Aw).

Tropical savanna climate or tropical wet and dry climate is a type of climate that corresponds to the Köppen climate classification categories "Aw" and '"As."

Tropical savanna climates have monthly mean temperature above 18°C in every month of the year and typically a pronounced dry season, with the driest month having precipitation less than 60 mm and also less than (100 − [total annual precipitation {mm}/25]). This latter fact is in direct contrast to a tropical monsoon climate, whose driest month sees less than 60 mm of precipitation but has more than (100 – [total annual precipitation {mm}/25]). In essence, a tropical savanna climate tends to either see less rainfall than a tropical monsoon climate or have more pronounced dry seasons than a tropical monsoon climate.

Versions

There are generally four versions of a tropical savanna climate:

• One form of the tropical savanna climate features distinct wet and dry seasons of relatively equal duration. Most of the region’s annual rainfall is experienced during the wet season and very little precipitation falls during the dry season.

• The second version of a tropical savanna climate features a lengthy dry season and a relatively short wet season. This version features seven or more dry season months and five or less wet season months. There are variations within this version. On one extreme, the region receives just enough precipitation during the short wet season to preclude it from a semi-arid climate classification. This drier variation of the tropical savanna climate is typically found adjacent to regions with semi-arid climates. On the other extreme, the climate features a lengthy dry season followed by a short but extremely rainy wet season. However, regions with this variation of the climate do not experience enough rainfall during the wet season to qualify as a tropical monsoon climate.

• The third version of a tropical savanna climate features a lengthy wet season and a relatively short dry season. This version features seven or more wet season months and five or less dry season months. This version’s precipitation pattern is similar to precipitation patterns observed in some tropical monsoon climates. However, regions with this variation of the climate do not experience enough rainfall during the wet season to qualify as a tropical monsoon climate.

• The fourth, rarer form of the tropical savanna climate features a dry season with a noticeable amount of rainfall followed by a rainy wet season. In essence, this version mimics the precipitation patterns more commonly found in a tropical monsoon climate. However, regions with this version of the climate fall short of a tropical monsoon climate categorization because it either does not receive enough precipitation during the dry season, or it does not receive enough annual precipitation.

Distribution

Rio de Janeiro
Climate chart (explanation)
J F M A M J J A S O N D     130   32 23     120   33 23     130   32 23     100   30 21     70   28 19     50   27 18     40   27 17     40   27 18     60   27 18     80   28 20     90   30 21     130   31 22 Average max. and min. temperatures in °C Precipitation totals in mm Source: Weatherbase [1]
Imperial conversion J F M A M J J A S O N D     5.1   90 73     4.7   91 73     5.1   90 73     3.9   86 70     2.8   82 66     2   81 64     1.6   81 63     1.6   81 64     2.4   81 64     3.1   82 68     3.5   86 70     5.1   88 72 Average max. and min. temperatures in °F Precipitation totals in inches

Tropical savanna climates are most commonly found in Africa, Asia and South America. The climate is also prevalent in sections of Central America, northern Australia and North America, specifically in sections of Mexico and the state of Florida in the United States. Most places that have this climate are found at the outer margins of the tropical zone, but occasionally an inner-tropical location (e.g., San Marcos, Antioquia, Colombia) also qualifies. Similarly, the Caribbean coast, eastward from the Gulf of Urabá on the Colombia–Panamá border to the Orinoco river delta, on the Atlantic ocean (ca. 4,000 km), have long dry periods (the extreme is the BSh climate (see below), characterised by very low, unreliable precipitation, present, for instance, in extensive areas in the Guajira, and Coro, western Venezuela, the northernmost peninsulas in South America, which receive <300 mm total annual precipitation, practically all in two or three months). This condition extends to the Lesser Antilles and Greater Antilles forming the Circumcaribbean dry belt. The length and severity of the dry season diminishes inland (southward); at the latitude of the Amazon river — which flows eastward, just south of the equatorial line — the climate is Af. East from the Andes, between the arid Caribbean and the ever-wet Amazon are the Orinoco river llanos or savannas, from where this climate takes its name.

Sometimes As is used in place of Aw if the dry season occurs during the time of higher sun and longer days. This is the case in parts of Hawaii, East Africa (Mombasa, Kenya), Sri Lanka (Trincomalee) and coastal regions of Northeastern Brazil (from Natal to Maceió), for instance. In most places that have tropical wet and dry climates, however, the dry season occurs during the time of lower sun and shorter days because of reduction of or lack of convection.

See also

• Tropics
• Köppen climate classification
• Tropical marine climate