Definition
According to climatologist Glenn G. Trewartha, a subtropical region should have at least eight months with a mean temperature of 10 °C (50.0 °F) or above. His revision of the Köppen climate classification assigns to such areas the letter C, while others zones encompassed in the original Köppen group C class would be considered part of group.
American climatologist John F. Griffiths in his book Applied climatology described the subtropical zone as having a coldest month of between 6 °C (42.8 °F) and 18 °C (64.4 °F) and assigning to this group the letter B, while the original B group of Köppen taxonomy would be spread over the various temperature-based groups.
German climatologists Carl Troll and Karlheinz Paffen defined warmgemäßigte Zonen ("Warm temperate zones") plain and hilly lands having an average temperature of the coldest month between 2 °C (35.6 °F) and 13 °C (55.4 °F) in Northern Hemisphere and between 6 °C (42.8 °F) and 13 °C (55.4 °F) in Southern Hemisphere, excluding oceanic and continental climates. According to Troll-Paffen climate classification, generally exist one a large subtropical zone named Warmgemäßigt-subtropisches Zonenklima (en: warm-temperate subtropical zone) divided into seven smaller areas.
According to E. Neef climate classification subtropical zone divided into two parts: Winterregenklima der Westseiten (en: Rainy winters of the west sides) and Subtropisches Ostseitenklima (en: Eastern subtropical climate).
According to Wilhelm Lauer & Peter Frankenberg climate classification subtropical zone divided into three parts: hoch-continental (high-continental), kontinental (continental) and maritim (maritime).
According to Siegmund/Frankenberg climate classification, subtropical is one of six climate zones in the world.
Read more about this topic: Subtropics
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