Tropical climate

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Locations of tropical climates, with subtypes.
Intertropical Convergence Zone vertical velocity at 500 hPa, July average in units of pascals per second. Ascent (negative values) is equator; descent (positive values) is more diffuse.

A tropical climate in the Köppen climate classification is a non-arid climate in which all twelve months have mean temperatures of at least 18 °C (64 °F). In tropical climates there are often only two seasons: a wet season and a dry season. Tropical climates are frost-free and changes in the solar angle are small. In tropical climates temperature remains relatively constant (hot) throughout the year.


Within the tropical climate zone there are distinct varieties based on precipitation:

Tropical rainforest climate[edit]

In the Tropical rainforest climate (Af):[1] all twelve months have an average precipitation of at least 60 mm (2.4 in). These climates usually occur within 5–10° latitude of the equator. In some eastern coast areas, they may extend to as much as over 26° away from the equator. This climate is dominated by the doldrums Low Pressure System all year round, and therefore has no natural seasons.

Tropical monsoon climate[edit]

The Tropical monsoon climate (Am):[1] is a type of climate that is common in South and Southeast Asia and in South and Central America, as well as part of Africa and Australia. It is dominated by the monsoon winds which change direction according to the seasons. This climate has a driest month (which nearly always occurs at or soon after the "winter" solstice for that side of the equator) with rainfall less than 60 millimetres (2.4 in), but more than (100 − [total annual precipitation {mm}/25]).

Tropical wet and dry climate[edit]

The Tropical wet and dry or savanna climate (Aw):[1] These climates generally have a pronounced dry season, with the driest month having precipitation less than 60 millimetres (2.4 in) and less than (100 − [total annual precipitation {mm}/25]).


Owing to different causes certain places within the tropics do not have a tropical climate, such as some desert areas and alpine regions.

  • Examples:
    • Southern part of Arabian Peninsula.
    • The Sahara Desert.
    • Alpine regions of the tropics. Mountaintops within the tropics, e.g. Mount Kenya, can be cold. However, like lowlands in the tropics (and unlike cold winter temperate zone regions), there is little seasonal variation of temperature.

Intertropical Convergence Zone[edit]

Because of the effect of sun angle on climate most areas within the tropics are hot year-round, with diurnal variations in temperature exceeding seasonal variations. Seasonal variations in tropical climate are dominated by changes in precipitation, which are in turn largely influenced by the tropical rain belt or Intertropical Convergence Zone (ITCZ), a portion of the Hadley cell. The ITCZ is shown, for July average, in the graphic. Areas of ascending air have heavy rainfall; areas of descending air are dry. The ITCZ somewhat follows the solar equator throughout the year, but with geographical variations, and in some areas (India) is heavily influenced by local large-scale monsoons.

See also[edit]


  1. ^ a b c McKnight, Tom L; Hess, Darrel (2000). "Climate Zones and Types: The Köppen System". Physical Geography: A Landscape Appreciation. Upper Saddle River, NJ: Prentice Hall. pp. 205–211. ISBN 0-13-020263-0. 
  2. ^ Linacre, Edward; Bart Geerts (1997). Climates and Weather Explained. London: Routledge. p. 379. ISBN 0-415-12519-7. 
  3. ^ "CHAPTER 7: Introduction to the Atmosphere". Retrieved 2008-07-15. 

External links[edit]