Tropical rainforest climate
      
Worldwide zones of Tropical rainforest climate (Af).
A tropical rainforest climate, also known as an equatorial climate, is another climate name for tropical climate usually (but not always) found along the equator. Regions with this climate typically feature tropical rainforests, and it is designated Af by the Köppen climate classification.
Description
Tropical rainforests have a type of tropical climate in which there is no dry season  – all months have an average precipitation value of at least 60 mm. Tropical rainforests have no summer or winter; it is typically hot and wet throughout the year and rainfall is both heavy and frequent. One day in an equatorial climate can be very similar to the next, while the change in temperature between day and night may be larger than the average change in temperature along the year.[1]
Distribution

Upland rainforest in Borneo. Sabah, Malaysia
 A tropical rainforest is usually found at latitudes within ten degrees North and South of the equator, which are dominated by the Intertropical Convergence Zone. The climate is most commonly found in Southeast Asia, Central Africa and South America. However, tropical microclimates are found in many other regions (e.g. far North Queensland), while not everywhere along the equatorial region features a tropical rainforest climate.
Some of the places that have this rainforests are indeed uniformly and monotonously wet throughout the year (e.g., the northwest Pacific coast of South and Central America, from Ecuador to Costa Rica, see for instance, Andagoya, Colombia), but in many cases the period of higher sun and longer days is distinctly driest (as at Palembang, Indonesia) or the time of lower sun and shorter days may have more rain (as at Sitiawan, Malaysia).
Additionally, while tropical rainforest climates are typically located near the equator (hence the alternate name “equatorial climate”), there are a number of instances where the climate is found some distance away from the equator. For instance, Santos, Brazil and Fort Lauderdale, USA are not only far removed from the equator, but are actually located just outside the tropics. Yet both of these cities feature a tropical rainforest climate, albeit with noticeably cooler and warmer periods of the year.
Notable cities with Tropical rainforest climates
| Africa North America   Punta Gorda, Belize  Limón, Costa Rica  Higüey, Dominican Republic  Puerto Barrios, Guatemala  La Ceiba, Honduras  Port Antonio, Jamaica  Bluefields, Nicaragua  Changuinola, Panama  Hilo, United States  Kapaa, United States  West Palm Beach, United States
 South America   Rurrenabaque, Bolivia  Belém, Brazil  Macaé, Brazil  Salvador, Brazil  Florencia, Colombia  Medellín, Colombia  Puyo, Ecuador  Saint-Laurent-du-Maroni, French Guiana  Georgetown, Guyana  Iquitos, Peru  Paramaribo, Suriname  San Carlos del Zulia, Venezuela
 
 | Asia   Bandar Seri Begawan, Brunei  Banda Aceh, Indonesia  Bandung, Indonesia  Banjarmasin, Indonesia  Biak, Indonesia  Bogor, Indonesia  Medan, Indonesia  Padang, Indonesia  Palangkaraya, Indonesia  Palembang, Indonesia  Pekanbaru, Indonesia  Pontianak, Indonesia  Samarinda, Indonesia  Tanjung Selor, Indonesia  Alor Setar, Malaysia  George Town, Malaysia  Ipoh, Malaysia  Johor Bahru, Malaysia  Kota Kinabalu, Malaysia  Kuala Lumpur, Malaysia  Kuala Terengganu, Malaysia  Kuching, Malaysia  Malacca City, Malaysia  Miri, Malaysia  Petaling Jaya, Malaysia  Shah Alam, Malaysia  Tabubil, Papua New Guinea  Davao City, Philippines  Polomolok, Philippines  Tacloban, Leyte, Philippines  Singapore  Colombo, Sri Lanka  Nakhon Si Thammarat, Thailand  Su-ngai Kolok, Thailand
 Oceania | 
 
 Examples 
| Western Samoa | 
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| Climate chart (explanation) | 
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| Paramaribo, Suriname | 
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| Climate chart (explanation) | 
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| J | F | M | A | M | J | J | A | S | O | N | D |  
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| Imperial conversion | 
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| Mbandaka, DR Congo | 
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| Climate chart (explanation) | 
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| J | F | M | A | M | J | J | A | S | O | N | D |  
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| Imperial conversion | 
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| Biak, Indonesia | 
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| Climate chart (explanation) | 
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| J | F | M | A | M | J | J | A | S | O | N | D |  
|  |  |  |  |  |  |  |  |  |  |  |  |  | Average max. and min. temperatures in °C |  | Precipitation totals in mm |  | Source: |  | 
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| Imperial conversion | 
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| Kuching, Malaysia | 
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| Climate chart (explanation) | 
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| J | F | M | A | M | J | J | A | S | O | N | D |  
|  |  |  |  |  |  |  |  |  |  |  |  |  | Average max. and min. temperatures in °C |  | Precipitation totals in mm |  | Source: Monthly Statistical Bulletin Sarawak |  | 
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| Imperial conversion | 
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 | J | F | M | A | M | J | J | A | S | O | N | D |  
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| Quibdó, Colombia | 
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| Climate chart (explanation) | 
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| J | F | M | A | M | J | J | A | S | O | N | D |  
|  |  |  |  |  |  |  |  |  |  |  |  |  | Average max. and min. temperatures in °C |  | Precipitation totals in mm |  | Source: |  | 
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| Imperial conversion | 
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 | J | F | M | A | M | J | J | A | S | O | N | D |  
|  |  |  |  |  |  |  |  |  |  |  |  |  | Average max. and min. temperatures in °F |  | Precipitation totals in inches |  | 
See also
References
- ↑  McKnight, Tom L; Hess, Darrel (2000). "Climate Zones and Types". Physical Geography: A Landscape Appreciation. Upper Saddle River, NJ: Prentice Hall. pp. 205–8. ISBN 0-13-020263-0. 
 
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 Humid continental (Dfa, Dwa, Dfb, Dwb, Dsa, Dsb) Subarctic (Dfc, Dwc, Dfd, Dwd, Dsc, Dsd)
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