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  2. File:ClimateMap World.png - Wikipedia

    en.wikipedia.org/wiki/File:ClimateMap_World.png

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  3. File:Map world climate zones (simplified to 10)-fr.svg ...

    en.wikipedia.org/wiki/File:Map_world_climate...

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  4. File:Trewartha climate classification world map.png - Wikipedia

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  5. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    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

  6. Geographical zone - Wikipedia

    en.wikipedia.org/wiki/Geographical_zone

    The five main latitude regions of Earth's surface comprise geographical zones, [1] divided by the major circles of latitude. The differences between them relate to climate. They are as follows: The North Frigid Zone, between the North Pole at 90° N and the Arctic Circle at 66°33′50.3″ N, covers 4.12% of Earth's surface.

  7. Category:Climate zones - Wikipedia

    en.wikipedia.org/wiki/Category:Climate_zones

    Tropics (12 C, 22 P) Pages in category "Climate zones" The following 11 pages are in this category, out of 11 total. This list may not reflect recent changes. H.

  8. Climate classification - Wikipedia

    en.wikipedia.org/wiki/Climate_classification

    An oceanic climate is typically found along west coasts in higher middle latitudes of all the world's continents, and in southeastern Australia, and is accompanied by plentiful precipitation year-round, cool summers, and small annual ranges of temperatures. Most climates of this type are found from 45 latitude to 55 latitude.

  9. List of life zones by region - Wikipedia

    en.wikipedia.org/wiki/List_of_life_zones_by_region

    The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.