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The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
The Trewartha system attempts to redefine the middle latitudes to be closer to vegetation zoning and genetic climate systems. The Trewartha climate classification changes were seen as most effective on the large landmasses in Asia and North America , where many areas fall into a single group ( C ) in the Köppen–Geiger system. [ 27 ]
The Trewartha climate classification (TCC), or the Köppen–Trewartha climate classification (KTC), is a climate classification system first published by American geographer Glenn Thomas Trewartha in 1966. It is a modified version of the Köppen–Geiger system, created to answer some of its deficiencies. [1]
Hydrology and Earth System Sciences: "Updated world map of the Köppen-Geiger climate classification" (Supplement) map in PDF (Institute for Veterinary Public Health) Legend explanation; Author: Peel, M. C., Finlayson, B. L., and McMahon, T. A. (University of Melbourne) Enhanced, modified, and vectorized by Ali Zifan.
The system isn't perfect, but it does help chart out the range of climates and weather experiences around the worldand what to expect from Mother Nature in different regions.
Ali Zifan (Enhanced, modified, and vectorized). Other versions: Köppen climate classification. Köppen climate classification (vector conversion) Regions of the world.
Hydrology and Earth System Sciences: "Updated world map of the Köppen-Geiger climate classification" (Supplement) Author: Peel, M. C., Finlayson, B. L., and McMahon, T. A. (University of Melbourne) Enhanced, modified, and vectorized by Ali Zifan. Permission (Reusing this file)
A humid subtropical climate is a subtropical-temperate climate type, characterized by long and hot summers, and cool to mild winters. 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, and equatorward from either humid continental (in North America and Asia ...