Humid subtropical climate in Li River, China As such, the climate can be said to exhibit somewhat different features depending on whether it is found inland, or in a maritime position. While many subtropical climates tend to be located at or near coastal locations, in some cases, they extend inland, most notably in China and the United States, where they exhibit more pronounced seasonal variations and sharper contrasts between summer and winter, as part of a gradient between the hotter tropical climates of the southern coasts and the colder continental climates to the north and further inland. In this classification, climates are termed humid subtropical when they have at least 8 months with a mean temperature above 10 ☌ (50 ☏). The humid subtropical climate classification was officially created under the Trewartha climate classification. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. This climate features mean temperature in the coldest month between 0 ☌ (32 ☏) (or −3 ☌ (27 ☏)) and 18 ☌ (64 ☏) and mean temperature in the warmest month 22 ☌ (72 ☏) or higher. Under the Köppen climate classification, Cfa and Cwa climates are either described as humid subtropical climates or warm temperate climates. It is also known as warm temperate climate in some climate classifications. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates. A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters.
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