
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. They experience high mean annual temperatures, small temperature ranges, and rain that falls throughout the year. Regions with this climate are typically designated Af by the Köppen climate classification. A tropical rainforest climate is typically hot, very humid, and wet with no dry season.

Description
Tropical rainforests have a type of tropical climate (with an average temperature of at least 18 C or 64.4 F in their coldest month) in which there is no dry season—all months have an average precipitation value of at least 60 mm (2.4 in). There are no distinct wet or dry seasons as rainfall is high throughout the months. One day in a tropical rainforest 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 during the year.
Equatorial climates and tropical trade-wind climates
When tropical rainforest climates are more dominated by the Intertropical Convergence Zone (ITCZ) than the trade winds (and with no or rare cyclones), so usually located near the equator, they are also called equatorial climates. Otherwise, when they are more dominated by the trade winds than the ITCZ, they are called tropical trade-wind climates. In pure equatorial climates, the atmospheric pressure is almost constantly low so the horizontal pressure gradient is low. Consequently, the winds are rare and usually weak (except sea and land breezes in coastal areas) while in tropical trade-wind climates, often located at higher latitudes than the equatorial climates, the wind is almost permanent which incidentally explains why rainforest formations are impoverished compared to those of equatorial climates due to their necessary resistance to strong winds accompanying tropical disturbances.
Cities with tropical rainforest climates
Asia
Oceania
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Mbandaka, DR Congo | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Pontianak, Indonesia | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Kuala Lumpur, Malaysia | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Davao, Philippines | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Quibdó, Colombia | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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See also
- Tropics
- Monsoon climate
- Tropical savanna climate
- Köppen climate classification
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 978-0-13-020263-5.
- Climatologie Pierre Estienne Alain Godard, pages 309 and 316
- Seidel, Dian J.; Fu, Qiang; Randel, William J.; Reichler, Thomas J. (January 2008). "Widening of the tropical belt in a changing climate". Nature Geoscience. 1 (1): 21–24. Bibcode:2008NatGe...1...21S. doi:10.1038/ngeo.2007.38. ISSN 1752-0908.
- "Nicobar Islands rain forests". Terrestrial Ecoregions. World Wildlife Fund.
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 They experience high mean annual temperatures small temperature ranges and rain that falls throughout the year Regions with this climate are typically designated Af by the Koppen climate classification A tropical rainforest climate is typically hot very humid and wet with no dry season Worldwide zones of tropical rainforest climate Af DescriptionBorneo with the typical vegetation of tropical forests Amazon rainforest Manaus Brazil Tropical rainforests have a type of tropical climate with an average temperature of at least 18 C or 64 4 F in their coldest month in which there is no dry season all months have an average precipitation value of at least 60 mm 2 4 in There are no distinct wet or dry seasons as rainfall is high throughout the months One day in a tropical rainforest 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 during the year Equatorial climates and tropical trade wind climates When tropical rainforest climates are more dominated by the Intertropical Convergence Zone ITCZ than the trade winds and with no or rare cyclones so usually located near the equator they are also called equatorial climates Otherwise when they are more dominated by the trade winds than the ITCZ they are called tropical trade wind climates In pure equatorial climates the atmospheric pressure is almost constantly low so the horizontal pressure gradient is low Consequently the winds are rare and usually weak except sea and land breezes in coastal areas while in tropical trade wind climates often located at higher latitudes than the equatorial climates the wind is almost permanent which incidentally explains why rainforest formations are impoverished compared to those of equatorial climates due to their necessary resistance to strong winds accompanying tropical disturbances Cities with tropical rainforest climatesAsia Malacca Car Nicobar India Balikpapan Indonesia Medan Indonesia Palembang Indonesia Ishigaki Japan Kuching Malaysia Johor Bahru Malaysia Kuala Lumpur Malaysia Davao City Philippines Polomolok Philippines Tacloban Leyte Philippines Singapore Colombo Sri Lanka Ratnapura Sri Lanka Sri Jayawardenepura Kotte Sri Lanka Orchid Island Taiwan Nakhon Si Thammarat Thailand Oceania Pago Pago American Samoa Tubuai Austral Islands Innisfail Queensland Australia Palikir Federated States of Micronesia Suva Fiji Hanga Roa Easter Island Chile Hagatna Guam Atuona French Polynesia Mata Utu French Polynesia Papeete French Polynesia Tarawa Kiribati Majuro Marshall Islands Alofi Niue New Zealand Koror Palau Tabubil Papua New Guinea Lae Papua New Guinea Pitcairn Island Apia Samoa Honiara Solomon Islands Nuku alofa Tonga Funafuti Tuvalu Hilo Hawaii United States Port Vila Vanuatu Africa Moroni Comoros Kisumu Kenya Harper Liberia Antalaha Madagascar Manakara Madagascar Toamasina Madagascar Victoria Seychelles Kampala Uganda Americas Punta Gorda Belize Hamilton Bermuda Villa Tunari Bolivia Belem Brazil Macae Brazil Salvador Brazil Buenaventura Valle del Cauca Colombia Florencia Colombia Leticia Colombia Cocos Island Costa Rica Limon Costa Rica Higuey Dominican Republic Puyo Ecuador Saint Laurent du Maroni French Guiana Pointe a Pitre Guadeloupe Puerto Barrios Guatemala Georgetown Guyana La Ceiba Honduras Port Antonio Jamaica Bluefields Nicaragua Changuinola Panama Iquitos Peru Lelydorp Suriname Paramaribo Suriname Scarborough Trinidad and Tobago West Palm Beach Florida United States Fort Lauderdale Florida United States Paramaribo SurinameClimate chart explanation J F M A M J J A S O N D 200 30 22 140 30 22 150 30 22 210 31 22 290 30 23 290 31 22 230 31 22 170 32 23 90 32 23 90 33 23 120 32 23 180 30 22 Average max and min temperatures in C Precipitation totals in mmSource 1 Imperial conversionJFMAMJJASOND 7 9 86 72 5 5 86 72 5 9 86 72 8 3 88 72 11 86 73 11 88 72 9 1 88 72 6 7 90 73 3 5 90 73 3 5 91 73 4 7 90 73 7 1 86 72 Average max and min temperatures in F Precipitation totals in inchesMbandaka DR CongoClimate chart explanation J F M A M J J A S O N D 80 31 19 100 32 20 150 32 20 140 31 20 130 31 20 110 30 19 100 30 17 100 29 17 200 30 19 210 30 19 190 30 19 120 30 19 Average max and min temperatures in C Precipitation totals in mmSource 2 Imperial conversionJFMAMJJASOND 3 1 88 66 3 9 90 68 5 9 90 68 5 5 88 68 5 1 88 68 4 3 86 66 3 9 86 63 3 9 84 63 7 9 86 66 8 3 86 66 7 5 86 66 4 7 86 66 Average max and min temperatures in F Precipitation totals in inchesPontianak IndonesiaClimate chart explanation J F M A M J J A S O N D 260 32 23 215 33 23 254 33 23 292 33 23 256 33 23 212 33 23 201 33 22 180 33 23 295 33 23 329 33 23 400 32 23 302 32 22 Average max and min temperatures in C Precipitation totals in mmSource 3 Imperial conversionJFMAMJJASOND 10 90 73 8 5 91 73 10 91 73 11 92 74 10 91 74 8 3 92 74 7 9 91 72 7 1 92 73 12 91 73 13 91 73 16 90 73 12 90 72 Average max and min temperatures in F Precipitation totals in inchesKuala Lumpur MalaysiaClimate chart explanation J F M A M J J A S O N D 227 33 24 193 33 24 270 34 25 302 34 25 230 34 25 146 33 25 165 33 24 174 33 25 220 33 24 284 33 24 356 32 24 281 32 24 Average max and min temperatures in C Precipitation totals in mmSource Monthly Statistical Bulletin SarawakImperial conversionJFMAMJJASOND 8 9 91 75 7 6 92 75 11 93 76 12 93 76 9 1 92 77 5 7 92 77 6 5 91 76 6 9 91 76 8 7 91 76 11 91 76 14 90 75 11 90 75 Average max and min temperatures in F Precipitation totals in inchesDavao PhilippinesClimate chart explanation J F M A M J J A S O N D 140 31 23 109 31 23 108 32 24 125 33 24 159 33 25 187 32 24 165 32 24 170 32 24 170 32 24 175 32 24 138 32 24 113 31 24 Average max and min temperatures in C Precipitation totals in mmSource 4 Imperial conversionJFMAMJJASOND 5 5 87 74 4 3 88 74 4 3 90 74 4 9 91 76 6 2 91 76 7 4 89 76 6 5 89 75 6 7 89 75 6 7 89 75 6 9 90 75 5 4 90 75 4 4 89 75 Average max and min temperatures in F Precipitation totals in inchesQuibdo ColombiaClimate chart explanation J F M A M J J A S O N D 579 30 23 505 30 23 526 30 23 655 31 23 776 31 23 762 31 23 803 31 23 852 31 23 702 31 23 654 30 23 728 30 23 589 30 23 Average max and min temperatures in C Precipitation totals in mmSource 5 Imperial conversionJFMAMJJASOND 23 86 73 20 86 74 21 87 74 26 87 74 31 88 74 30 88 73 32 88 73 34 88 73 28 87 73 26 87 73 29 86 73 23 85 73 Average max and min temperatures in F Precipitation totals in inchesSee alsoTropics Monsoon climate Tropical savanna climate Koppen climate classificationReferencesMcKnight Tom L Hess Darrel 2000 Climate Zones and Types Physical Geography A Landscape Appreciation Upper Saddle River NJ Prentice Hall pp 205 8 ISBN 978 0 13 020263 5 Climatologie Pierre Estienne Alain Godard pages 309 and 316 Seidel Dian J Fu Qiang Randel William J Reichler Thomas J January 2008 Widening of the tropical belt in a changing climate Nature Geoscience 1 1 21 24 Bibcode 2008NatGe 1 21S doi 10 1038 ngeo 2007 38 ISSN 1752 0908 Nicobar Islands rain forests Terrestrial Ecoregions World Wildlife Fund