Tropical_monsoon_climate
Tropical monsoon climate
Climate subtype in the Köppen climate classification system
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 Failed to parse (unknown function "\franc"): {\textstyle 100-\left(\franc{Total\ Annual\ Precipitation\ (mm)}{25}\right)} .[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 Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "http://localhost:6011/en.wikipedia.org/v1/":): {\textstyle 100-\left(\franc{Total\ Annual\ Precipitation\ (mm)}{25}\right)} 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]