Geographical zone
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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' N, covers 4.12% of Earth's surface.
- The North Temperate Zone, between the Arctic Circle at 66° 33' N and the Tropic of Cancer at 23° 27' N, covers 25.99% of Earth's surface.
- The Torrid Zone, between the Tropic of Cancer at 23° 27' N and the Tropic of Capricorn at 23° 27' S, covers 39.78% of Earth's surface.
- The South Temperate Zone, between the Tropic of Capricorn at 23° 27' S and the Antarctic Circle at 66° 33' S, covers 25.99% of Earth's surface.
- The South Frigid Zone, from the Antarctic Circle at 66° 33' S and the South Pole at 90° S, covers 4.12% of Earth's surface.
On the basis of latitudinal extent, the globe is divided into three broad heat zones.
Torrid zone
The Torrid is also known as the Tropics. This zone is bounded on the north by the Tropic of Cancer and on the south by the Tropic of Capricorn; these latitudes mark the northern and southern extremes in which the sun passes[a] directly overhead. This happens once annually on these cusps, but in Tropics proper, the sun passes overhead twice a year.
Within the Northern Tropics, the sun passes overhead its first time for that year before the June solstice, at which time it does so as to the Tropic of Cancer. It passes over these latitudes in turn again, on its apparent southward journey, to and before the September Equinox. After then, the center of the sun at the high point, the zenith, of the sky (which makes for the subsolar point beneath) aligns with successive latitudes in the Southern Tropics. The sun passes overhead of these then does so once per year for the Tropic of Capricorn at the December solstice, then passes back again over those latitudes to return to the Equator for the March Equinox.
Temperate zones
In the two temperate zones, consisting of the tepid latitudes, the Sun is never directly overhead, and the climate is mild, generally ranging from warm to cool. The four annual seasons, spring, summer, autumn and winter, occur in these areas. The North Temperate Zone includes Europe, Northern Asia, and North and Central America. The South Temperate Zone includes Southern Australasia, southern South America, and Southern Africa.
Frigid zones
The two frigid zones, or polar regions, experience the midnight sun and the polar night for part of the year – at the edge of the zone there remains one day, the winter solstice, when the Sun is too low to rise, and one day at the summer solstice when the sun remains above the horizon for 24 hours. In the center of the zone (the pole) the day is one year long with six months of daylight and six months of night. The frigid zones are the coldest regions of Earth and are generally covered in ice and snow. It receives slanting rays of the sun as this region lies farthest from the equator. Summer season in this region lasts for about 2 to 3 months and there is almost 24 hour sunlight during summer. The sun's rays are always slanting so provide less heat per horizontal surface area.
History
The concept of a geographical zone was first hypothesized by the ancient Greek scholar Parmenides[2] and lastingly modified by Aristotle.[3] Both philosophers theorized the Earth divided into three types of climatic zones based on their distance from the equator.
Like Parmeneides, thinking that the area near the equator was too hot for habitation, Aristotle dubbed the region around the equator (from 23.5° N to 23.5° S) the "Torrid Zone." Both philosophers reasoned the region from the Arctic Circle to the pole to be permanently frozen. This region, thought uninhabitable, was called the "Frigid Zone." The only area believed to be habitable was the northern "Temperate Zone" (the southern one not having been discovered), lying between the "Frigid Zones" and the "Torrid Zone". However, humans have inhabited almost all climates on Earth, including inside the Arctic Circle.
As knowledge of the Earth's geography improved, a second "Temperate Zone" was discovered south of the equator, and a second "Frigid Zone" was discovered around the Antarctic. Although Aristotle's map was oversimplified, the general idea was correct. Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.
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See also
- Circle of latitude
- Climate classification
- Clime
- Hardiness zone
- Polar regions of Earth
- Subtropics
- Temperate climate
- Tropics
References and footnotes
- ^ "The Five Geographical Zones Of The World". WorldAtlas. Retrieved 2019-09-17.
- ^ Strab. 2,2,1-2 in: A. H. Coxon and R. D. McKirahan (eds), The Fragments of Parmenides: A Critical Text With Introduction, and Translation, the Ancient Testimonia and a Commentary, 2nd edn (Phresis: Supplementary Volumes 3; Assen, Dover (NH), 2009), p. 160.
- ^ Aristotle, Meteorology, Bekker numbers 362a33-362b29
- ^ The "Sun passing", "reaching" or similar, implying a movement of the sun, is – in the widest context – conflating subject with object.
Astronomy, although it treats the Sun from the Earth's perspective with global, cyclical, limited northward and southern migration (in the sky, the celestial sphere), proves this is due to the Earth's axial tilt, and its unlimited east-west movement is due to the earth's orbit. If seeing and analyzing the Earth and Sun in space, the Earth moves such that a geographical zone faces the Sun more or less at a certain date, or moves to align beneath the sun, due to tilt, a particular latitude.
