Temperature zone: Difference between revisions

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|Meaning=Very generally, a portion of the earth's surface defined by relatively uniform  [[temperature]] characteristics, and usually bounded by selected values of some measure of temperature  or temperature effect.
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|Explanation=All of the following may be considered "temperature zones": A. Supan's 1879 [[hot belt]], [[temperate belt|temperate  belt]], and [[cold cap]]; W. K&#x000f6;ppen's 1936 [[tropical rainy climates]], [[temperate rainy climates]], [[snow  forest climates]], and [[polar climates]]; C. W. Thornthwaite's 1931 [[temperature provinces]]. It is  occasionally used for a vertical subdivision of [[thermal belts]] in mountainous terrain. <br/>''See also''  [[mathematical climate]], [[solar climate]].<br/> Supan, A. 1879. Die Temperaturzonen der Erde. Petermanns Geog. Mitt.. 25. 349&ndash;358. <br/> K&#x000f6;ppen, W. P., and R. Geiger 1930&ndash;1939. Handbuch der Klimatologie. Berlin: Gebruder Borntraeger, 6 vols. <br/> Thornthwaite, C. W. 1931. The climates of North America according to a new classification. Geogr. Rev..  21. 633&ndash;655.  
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== temperature zone ==
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<div class="definition"><div class="short_definition">Very generally, a portion of the earth's surface defined by relatively uniform  [[temperature]] characteristics, and usually bounded by selected values of some measure of temperature  or temperature effect.</div><br/> <div class="paragraph">All of the following may be considered "temperature zones": A. Supan's 1879 [[hot belt]], [[temperate belt|temperate  belt]], and [[cold cap]]; W. K&#x000f6;ppen's 1936 [[tropical rainy climates]], [[temperate rainy climates]], [[snow  forest climates]], and [[polar climates]]; C. W. Thornthwaite's 1931 [[temperature provinces]]. It is  occasionally used for a vertical subdivision of [[thermal belts]] in mountainous terrain. <br/>''See also''  [[mathematical climate]], [[solar climate]].</div><br/> </div><div class="reference">Supan, A. 1879. Die Temperaturzonen der Erde. Petermanns Geog. Mitt.. 25. 349&ndash;358. </div><br/> <div class="reference">K&#x000f6;ppen, W. P., and R. Geiger 1930&ndash;1939. Handbuch der Klimatologie. Berlin: Gebruder Borntraeger, 6 vols. </div><br/> <div class="reference">Thornthwaite, C. W. 1931. The climates of North America according to a new classification. Geogr. Rev..  21. 633&ndash;655. </div><br/>
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Latest revision as of 10:08, 28 March 2024

Very generally, a portion of the earth's surface defined by relatively uniform temperature characteristics, and usually bounded by selected values of some measure of temperature or temperature effect.

All of the following may be considered "temperature zones": A. Supan's 1879 hot belt, temperate belt, and cold cap; W. Köppen's 1936 tropical rainy climates, temperate rainy climates, snow forest climates, and polar climates; C. W. Thornthwaite's 1931 temperature provinces. It is occasionally used for a vertical subdivision of thermal belts in mountainous terrain.
See also mathematical climate, solar climate.
Supan, A. 1879. Die Temperaturzonen der Erde. Petermanns Geog. Mitt.. 25. 349–358.
Köppen, W. P., and R. Geiger 1930–1939. Handbuch der Klimatologie. Berlin: Gebruder Borntraeger, 6 vols.
Thornthwaite, C. W. 1931. The climates of North America according to a new classification. Geogr. Rev.. 21. 633–655.

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