Essentials of Geography

Geographical Zones

Natural systems of climate, vegetation, and soil change substantially as one travels from the equator to the pole due largely to the latitudinal variation in energy input to the earth system. The early Greek scholar Aristotle was the first to divide the Earth into zones based on climate. His "torrid zone", thought to be too hot for human habitation, lay between 23.5^o N and 23.5^o S. Aristotle thought that the "temperate zones" between 23.5^o N - 66.5^o N and 23.5^o S - 66.5^o S were the only livable zones. From the arctic (66.5 N) and and antarctic circles (66.5 S) to the the poles (90 N and S) were the uninhabitable "frigid zones".

Figure 1.38a Torrid Zone Image Source: WikiMedia

Figure 1.38b Temperate Zones Image Source: WikiMedia

Figure 1.38c Frigid Zones Image Source: WikiMedia

Geographers continue to use latitudinal variation of climate characteristics as a way of dividing the Earth into fairly homogeneous geographical zones. These zones are:

Equatorial: 10^o N - 10^o S

Tropical:  10^oN - 25^oN and 10^oS - 25^oS

Subtropical: 25^oN - 35^oN and 25^oS - 35^oS
 
Midlatitude: 35^oN - 55^oN  and 35^oS - 55^oS

Subarctic: 55^oN - 60^oN

Subantarctic: 55^oS - 60^oS

Arctic: 60^oN - 75N^o

Antarctic: 60^oS - 75^oS

North Polar: 75^oN - 90^oN

South Polar: 75^oS - 90^oS

[Figure 1.39 Geographical Zones Not Available Yet]

The equatorial zone is characterized by warm temperatures and nearly uniform day length throughout the year. The boundary of the tropical zone lies close to the Tropic of Cancer (23.5^oN) and Capricorn (23.5^oS), the latitudinal limit where the Sun is directly over head at noon at different times of the year. The subtropical zone includes Aristotle's home of Greece, and seasonal changes in temperature become more pronounced. The temperate midlatitude zone is noted for is variable weather conditions. Large annual swings in temperature are characteristic of the subarctic and subantarctic zone where extensive areas of cold air form during winter and milder conditions prevail during summer. The coldest zones are the Arctic and Antarctic, where the Sun never rises above the horizon for several months at a time. Much of the light that does reach the surface is reflected off the light colored surfaces of the North (sea ice) and South (mostly glacial ice) poles. The coldest zones are the North and South Polar. Like the Arctic and Antarctic Zones, the Sun never rises above the horizon for many months of the year. The coldest temperatures are near the South Pole, far from any moderating influence of an ocean and the little light that does make it to the surface is reflected from glacier ice.

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For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
Date visited.  https://www.earthonlinemedia.com/ebooks/tpe_3e/title_page.html

Michael Ritter (tpeauthor@mac.com)
Last revised 6/5/12

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