Ajay Kumar (talk | contribs) Created a new article |
No edit summary |
||
| Line 1: | Line 1: | ||
{{Short description|Climate subtype in the Köppen climate classification system}} | {{Short description|Climate subtype in the Köppen climate classification system}} | ||
[[File: | [[File:Koppen-Geiger_Map_v2_Am_1991–2020.svg|thumb|upright=2|Worldwide zones of tropical monsoon climate (Am).]]An '''area of tropical monsoon climate''' (occasionally known as a '''sub-equatorial''', '''tropical wet climate''' or a '''tropical monsoon and trade-wind littoral climate''') is a [[tropical climate]] subtype that corresponds to the [[Köppen climate classification]] category '''''Am'''''. Tropical monsoon climates have monthly mean temperatures above {{convert|18|°C|0}} in every month of the year and a dry season.<ref name=McKnight>{{cite book | last1=McKnight | first1=Tom L | last2=Hess | first2=Darrel | year=2000 | chapter=Climate Zones and Types | title=Physical Geography: A Landscape Appreciation | location=Upper Saddle River, New Jersey | publisher=Prentice Hall | isbn=978-0-13-020263-5 | chapter-url-access=registration | chapter-url=https://archive.org/details/physicalgeographmckn | url-access=registration | url=https://archive.org/details/physicalgeographmckn }}</ref>{{rp|200–1}} The tropical monsoon climate is the intermediate climate between the wet Af (or [[tropical rainforest climate]]) and the drier Aw (or [[tropical savanna climate]]). | ||
A tropical monsoon climate's driest month has on average less than 60 mm, but more than <math display="inline">100-\left(\frac{Total\ Annual\ Precipitation\ (mm)}{25}\right)</math>.<ref name=McKnight /> This is in direct contrast to a [[tropical savanna climate]], whose driest month has less than 60 mm of precipitation and also less than <math display="inline">100-\left(\frac{Total\ Annual\ Precipitation\ (mm)}{25}\right)</math> of average monthly precipitation. In essence, a tropical monsoon climate tends to either have more rainfall than a tropical savanna climate or have less pronounced dry seasons. A tropical monsoon climate tends to vary less in temperature during a year than does a tropical savanna climate. This climate has | A tropical monsoon climate's driest month has on average less than 60 mm, but more than <math display="inline">100-\left(\frac{Total\ Annual\ Precipitation\ (mm)}{25}\right)</math>.<ref name=McKnight /> This is in direct contrast to a [[tropical savanna climate]], whose driest month has less than 60 mm of precipitation and also less than <math display="inline">100-\left(\frac{Total\ Annual\ Precipitation\ (mm)}{25}\right)</math> of average monthly precipitation. In essence, a tropical monsoon climate tends to either have more rainfall than a tropical savanna climate or have less pronounced dry seasons. A tropical monsoon climate tends to vary less in temperature during a year than does a tropical savanna climate. This climate has the driest month, which nearly always occurs at or soon after the winter solstice.<ref name=McKnight/> | ||
== | ==Varieties== | ||
There are generally two | There are generally two varieties of a tropical monsoon climate: | ||
* Less pronounced dry seasons. Regions with this variation of the tropical monsoon climate typically see copious amounts of rain during the wet season(s), usually in the form of frequent thunderstorms. Unlike most tropical savanna climates, a sizeable amount of precipitation also falls during the dry season(s). In essence, this version of the tropical monsoon climate generally has less pronounced dry seasons than tropical savanna climates. | * Less pronounced dry seasons. Regions with this variation of the tropical monsoon climate typically see copious amounts of rain during the wet season(s), usually in the form of frequent thunderstorms. Unlike most tropical savanna climates, a sizeable amount of precipitation also falls during the dry season(s), but not quite enough for a [[tropical rainforest climate|tropical rainforest]] classification. In essence, this version of the tropical monsoon climate generally has less pronounced dry seasons than tropical savanna climates. | ||
* Extraordinarily rainy wet seasons and pronounced dry seasons. This variation features pronounced dry seasons similar in length and character to dry seasons observed in tropical savanna climates. This is followed by a sustained period (or sustained periods) of extraordinary rainfall. In some instances, up to (and sometimes in excess of) 1,000 mm of precipitation is observed per month for two or more consecutive months. Tropical savanna climates generally do not see this level of sustained rainfall. | * Extraordinarily rainy wet seasons and pronounced dry seasons. This variation features pronounced dry seasons similar in length and character to dry seasons observed in tropical savanna climates. This is followed by a sustained period (or sustained periods) of extraordinary rainfall. In some instances, up to (and sometimes in excess of) 1,000 mm of precipitation is observed per month for two or more consecutive months. Tropical savanna climates generally do not see this level of sustained rainfall. | ||
==Area== | ==Area== | ||
[[File:AtardecerRioMAgdalena.jpg|thumb|[[Magdalena River]] at Honda, [[Colombia]].]] | [[File:AtardecerRioMAgdalena.jpg|thumb|[[Magdalena River]] at Honda, [[Colombia]].]] | ||
Tropical monsoon are most commonly found in [[Africa]] ([[West Africa|West]] and [[Central Africa]]), [[Asia]] ([[South Asia|South]] and [[Southeast Asia]]), | Tropical monsoon are most commonly found in [[Africa]] ([[West Africa|West]] and [[Central Africa]]), [[Asia]] ([[South Asia|South]] and [[Southeast Asia]]), northern [[South America]], and [[Central America]]. This climate also occurs in sections of the [[Caribbean]], [[North America]] ([[South Florida]]), and northern [[Australia]]. | ||
==Factors== | ==Factors== | ||
The major controlling factor over a tropical monsoon climate is its relationship to the [[monsoon]] circulation. The monsoon is a seasonal change in wind direction. In Asia, during the summer (or high-sun season) there is an onshore flow of air (air moving from ocean toward land). In the “winter” (or low-sun season) an offshore air flow (air moving from land toward water) is prevalent. The change in direction is due to the difference in the way water and land heat. | The major controlling factor over a tropical monsoon climate is its relationship to the [[monsoon]] circulation. The monsoon is a seasonal change in wind direction. In Asia, during the summer (or high-sun season) there is an onshore flow of air (air moving from ocean toward land). In the “winter” (or low-sun season) an offshore air flow (air moving from land toward water) is prevalent. The change in direction is due to the difference in the way water and land heat. | ||
Changing pressure patterns that affect the seasonality of precipitation also occur in Africa though it generally differs from the way it operates in Asia. During the high-sun season, the [[Intertropical convergence zone]] (ITCZ) induces rain. During the low-sun season, the subtropical high creates dry conditions. The monsoon climates of Africa, and the Americas for that matter, are typically located along | Changing pressure patterns that affect the seasonality of precipitation also occur in Africa, though it generally differs from the way it operates in Asia. During the high-sun season, the [[Intertropical convergence zone]] (ITCZ) induces rain. During the low-sun season, the subtropical high creates dry conditions. The monsoon climates of Africa, and the Americas for that matter, are typically located along trade wind coasts. | ||
==Countries and cities== | ==Countries and cities== | ||
{{col-begin|width=75%}} | |||
{{col-1-of-2}} | {{col-1-of-2}} | ||
'''Asia''' | '''Asia''' | ||
* [[ | * [[Chittagong]], Bangladesh | ||
* [[ | * [[Sylhet]], Bangladesh | ||
* [[ | * [[Sihanoukville (city)|Sihanoukville]], Cambodia | ||
* [[ | * [[Qionghai]], China | ||
* [[ | * [[Wanning]], China | ||
* [[ | * [[Kochi]], [[Kerala]], India | ||
* [[ | * [[Mangalore]], [[Karnataka]], India | ||
* [[Jakarta]], | * [[Thiruvananthapuram]], [[Kerala]], India | ||
* [[ | * [[Bandung]], Indonesia | ||
* [[ | * [[Jakarta]], Indonesia | ||
* [[ | * [[Makassar]], Indonesia | ||
* [[ | * [[Chichijima]], Japan | ||
* [[ | * [[Alor Setar]], [[Kedah]], Malaysia | ||
* [[ | * [[Langkawi]], Malaysia | ||
* [[ | * [[Malé]], Maldives | ||
* [[ | * [[Kulhudhuffushi]], Maldives | ||
* [[Quezon City]], | * [[Yangon]], Myanmar | ||
* [[ | * [[Calamba, Philippines|Calamba]], Philippines | ||
* [[ | * [[Manila, Philippines|Manila]], Philippines | ||
* [[ | * [[Quezon City]], Philippines | ||
* [[Taitung County|Taitung]], | * [[Batticaloa]], Sri Lanka | ||
* [[ | * [[Kaohsiung]], Taiwan | ||
*[[ | * [[Pingtung County|Pingtung]], Taiwan | ||
* [[ | * [[Taitung County|Taitung]], Taiwan | ||
* [[ | * [[Hat Yai]], Thailand | ||
* [[Narathiwat]], Thailand | |||
* [[Pattani, Thailand|Pattani]], Thailand | |||
* [[Cà Mau]], Vietnam | |||
* [[Da Nang]], Vietnam | |||
'''Oceania''' | |||
* [[Cairns]], [[Queensland]], Australia | |||
* [[Christmas Island]], Australia | |||
* [[Saipan, Northern Mariana Islands|Saipan]], Northern Mariana Islands | |||
{{col-2-of-2}} | {{col-2-of-2}} | ||
'''Africa''' | '''Africa''' | ||
* [[Bata, Equatorial Guinea]] | * [[Douala]], Cameroon | ||
* [[Conakry]], | * [[Bata, Equatorial Guinea|Bata]], Equatorial Guinea | ||
* [[ | * [[Conakry]], Guinea | ||
* [[ | * [[Monrovia]], Liberia | ||
* [[ | * [[Port Harcourt]], Nigeria | ||
* [[ | * [[Umuahia]], Nigeria | ||
* [[Freetown]], Sierra Leone | |||
'''The Americas''' | '''The Americas''' | ||
* [[ | * [[Recife]], [[Pernambuco]], Brazil | ||
* [[Barrancabermeja, Colombia|Barrancabermeja]], [[Colombia]] | * [[Macapá]], [[Amapá]], Brazil | ||
* [[ | * [[Barrancabermeja, Colombia|Barrancabermeja]], Colombia | ||
* [[ | * [[Villavicencio]], Colombia | ||
* [[San Juan, Puerto Rico]], [[United States | * [[Roseau]], Dominica | ||
* [[ | * [[Santo Domingo]], Dominican Republic | ||
* [[ | * [[Cayenne]], French Guiana (bordering on ''Af'') | ||
* [[ | * [[Coatzacoalcos]], Mexico | ||
* [[Villahermosa]], Mexico | |||
* [[Managua]], Nicaragua | |||
* [[Panama City]], Panama | |||
* [[Pucallpa]], Peru | |||
* [[San Juan, Puerto Rico]] | |||
* [[Miami]], [[Florida]], United States | |||
* [[Basseterre]], Saint Kitts and Nevis | |||
* [[Nassau, The Bahamas|Nassau]], The Bahamas (bordering on ''Aw'') | |||
* [[Port of Spain]], Trinidad and Tobago | |||
* [[Guanare]], Venezuela | |||
* [[Mérida (state)|Mérida]], Venezuela | |||
* [[Puerto Ayacucho]], Venezuela | |||
{{col-end}} | {{col-end}} | ||
===Select charts=== | ===Select charts=== | ||
{{climate chart | {{climate chart | ||
|[[ | |[[Manila]], Philippines | ||
|23.9|29.9|19.4 | |||
|26.2|30.7|21.9 | |||
|25.3|32.1|21.8 | |||
|26.7|33.8|23.4 | |||
|27.0|33.6|159.1 | |||
|26.5|32.8|253.3 | |||
|25.9|31.5|432.3 | |||
|25.9|31.0|476.1 | |||
|25.7|31.2|396.4 | |||
|25.7|31.4|220.6 | |||
|25.3|31.3|119.9 | |||
|24.6|30.3|98.5 | |||
|source=[[PAGASA]] | |||
|float=left | |||
|clear=none | |||
}} | |||
{{climate chart | |||
|[[Kaohsiung]], Taiwan | |||
|16.2 |24.2 |19.1 | |||
|17.2 |25.0 |17.7 | |||
|19.7 |27.0 |32.3 | |||
|22.8 |29.3 |68.4 | |||
|25.2 |31.0 |202.2 | |||
|26.3 |32.1 |416.2 | |||
|26.7 |32.7 |377.2 | |||
|26.3 |32.1 |512.4 | |||
|25.9 |31.8 |224.5 | |||
|24.2 |30.1 |53.4 | |||
|21.6 |28.1 |25.6 | |||
|17.9 |25.3 |19.2 | |||
|source=Climate Data<ref>{{cite web |title=Climate Kaohsiung City (Republic of China (Taiwan)) |url=https://en.climate-data.org/asia/republic-of-china/kaohsiung-city/kaohsiung-city-1054/ |archive-url=https://web.archive.org/web/20190221000525/https://en.climate-data.org/asia/republic-of-china/kaohsiung-city/kaohsiung-city-1054/ |archive-date=21 February 2019 |url-status=live |access-date=20 February 2019}}</ref> | |||
|float=left | |||
|clear=none | |||
}} | |||
{{climate chart | |||
|[[Chittagong]], Bangladesh | |||
|15|27|5 | |15|27|5 | ||
|19|30|28 | |19|30|28 | ||
| Line 90: | Line 145: | ||
{{climate chart | {{climate chart | ||
| [[Conakry]], | | [[Conakry]], Guinea | ||
|19 |32.2 |1 | |19 |32.2 |1 | ||
|20.2 |33.1 |1 | |20.2 |33.1 |1 | ||
| Line 110: | Line 165: | ||
{{climate chart | {{climate chart | ||
|[[ | |[[Jakarta]], Indonesia | ||
| 24.3 |30.5 |363 | |||
| 24.2 |30.6 |323 | |||
| 24.7 |31.8 |191 | |||
| 25.0 |32.4 |153 | |||
| 25.1 |32.7 |110 | |||
| 24.8 |32.5 |75 | |||
| 24.4 |32.4 |66 | |||
| 24.5 |32.5 |53 | |||
| 24.7 |32.8 |61 | |||
| 24.9 |32.8 |111 | |||
| 24.8 |32.3 |124 | |||
| 24.6 |31.4 |196 | |||
|source= BMKG<ref>{{cite web |url=https://www.staklimtangsel.id/images/rataunsurcuaca/rataunsurcuaca10.jpg |title=Climatological Average of Kemayoran Meteorological Station for 1981–2010 |publisher=Pondok Betung Climatological Station – Indonesian Bureau of Meteorology, Climatology, and Geophysics |accessdate=19 April 2021 |language=id |archive-date=21 April 2021 |archive-url=https://web.archive.org/web/20210421062556/https://www.staklimtangsel.id/images/rataunsurcuaca/rataunsurcuaca10.jpg |url-status=live }}</ref> | |||
|float = left | |||
|clear = none | |||
}} | |||
{{climate chart | |||
|[[Miami]], Florida, US | |||
| 15.1 | 24.0 | 51.1 | | 15.1 | 24.0 | 51.1 | ||
| 15.8 | 24.7 | 52.8 | | 15.8 | 24.7 | 52.8 | ||
Latest revision as of 18:14, 21 March 2026
An area of tropical monsoon climate (occasionally known as a sub-equatorial, tropical wet climate or a tropical monsoon and trade-wind littoral climate) is a tropical climate subtype that corresponds to the Köppen climate classification category Am. Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and a dry season.[1]:200–1 The tropical monsoon climate is the intermediate climate between the wet Af (or tropical rainforest climate) and the drier Aw (or tropical savanna climate).
A tropical monsoon climate's driest month has on average less than 60 mm, but more than .[1] This is in direct contrast to a tropical savanna climate, whose driest month has less than 60 mm of precipitation and also less than of average monthly precipitation. In essence, a tropical monsoon climate tends to either have more rainfall than a tropical savanna climate or have less pronounced dry seasons. A tropical monsoon climate tends to vary less in temperature during a year than does a tropical savanna climate. This climate has the driest month, which nearly always occurs at or soon after the winter solstice.[1]
Varieties[edit | edit source]
There are generally two varieties of a tropical monsoon climate:
- Less pronounced dry seasons. Regions with this variation of the tropical monsoon climate typically see copious amounts of rain during the wet season(s), usually in the form of frequent thunderstorms. Unlike most tropical savanna climates, a sizeable amount of precipitation also falls during the dry season(s), but not quite enough for a tropical rainforest classification. In essence, this version of the tropical monsoon climate generally has less pronounced dry seasons than tropical savanna climates.
- Extraordinarily rainy wet seasons and pronounced dry seasons. This variation features pronounced dry seasons similar in length and character to dry seasons observed in tropical savanna climates. This is followed by a sustained period (or sustained periods) of extraordinary rainfall. In some instances, up to (and sometimes in excess of) 1,000 mm of precipitation is observed per month for two or more consecutive months. Tropical savanna climates generally do not see this level of sustained rainfall.
Area[edit | edit source]

Tropical monsoon are most commonly found in Africa (West and Central Africa), Asia (South and Southeast Asia), northern South America, and Central America. This climate also occurs in sections of the Caribbean, North America (South Florida), and northern Australia.
Factors[edit | edit source]
The major controlling factor over a tropical monsoon climate is its relationship to the monsoon circulation. The monsoon is a seasonal change in wind direction. In Asia, during the summer (or high-sun season) there is an onshore flow of air (air moving from ocean toward land). In the “winter” (or low-sun season) an offshore air flow (air moving from land toward water) is prevalent. The change in direction is due to the difference in the way water and land heat.
Changing pressure patterns that affect the seasonality of precipitation also occur in Africa, though it generally differs from the way it operates in Asia. During the high-sun season, the Intertropical convergence zone (ITCZ) induces rain. During the low-sun season, the subtropical high creates dry conditions. The monsoon climates of Africa, and the Americas for that matter, are typically located along trade wind coasts.
Countries and cities[edit | edit source]
|
Asia
Oceania
|
Africa
The Americas
|
Select charts[edit | edit source]
| Manila, Philippines | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Kaohsiung, Taiwan | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Chittagong, Bangladesh | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Conakry, Guinea | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Jakarta, Indonesia | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Miami, Florida, US | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Climate chart (explanation) | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
See also[edit | edit source]
References[edit | edit source]
- ↑ 1.0 1.1 1.2 McKnight, Tom L; Hess, Darrel (2000). "Climate Zones and Types". Physical Geography: A Landscape Appreciation. Upper Saddle River, New Jersey: Prentice Hall. ISBN 978-0-13-020263-5.
- ↑ "Climate Kaohsiung City (Republic of China (Taiwan))". Archived from the original on 21 February 2019. Retrieved 20 February 2019.
- ↑ "Average Conditions - Chittagong, Bangladesh". BBC Weather. Archived from the original on 11 March 2006. Retrieved 25 June 2018.
- ↑ "Climatological Normals of Conakry". Hong Kong Observatory. Retrieved 2014-02-12.
- ↑ "Climatological Average of Kemayoran Meteorological Station for 1981–2010" (in Bahasa Indonesia). Pondok Betung Climatological Station – Indonesian Bureau of Meteorology, Climatology, and Geophysics. Archived from the original on 21 April 2021. Retrieved 19 April 2021.
- ↑ "Weather Information for Miami, Florida". World Meteorological Organization. Retrieved 25 June 2018.