Temperate rainy climate: Difference between revisions

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One of the major categories (the C climate) in W. K&#x000f6;ppen's 1936 [[climatic classification|climatic  classification]]. These climates have a coldest-month [[mean temperature]] of less than 18&#x000b0;C (64.4&#x000b0;F)  and greater than -3&#x000b0;C (26.6&#x000b0;F), with a warmest-month mean temperature of more than 10&#x000b0;C  (50&#x000b0;F).<br/> These limits distinguish it, respectively, from [[tropical rainy climates]], [[snow forest climates]],  and [[tundra climates]]. It is separated from the [[dry climates]] by a function of annual [[temperature]]  and [[precipitation]]. In C. W. Thornthwaite's 1931 classifications, the humid or moist subhumid  and [[mesothermal climates]] would very closely correspond to the above. <br/>''See'' formulas under [[steppe climate|steppe  climate]].<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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== temperate rainy climate ==
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<div class="definition"><div class="short_definition">One of the major categories (the C climate) in W. K&ouml;ppen's 1936 [[climatic  classification]]. These climates have a coldest-month [[mean temperature]] of less than 18&deg;C (64.4&deg;F)  and greater than &minus;3&deg;C (26.6&deg;F), with a warmest-month mean temperature of more than 10&deg;C  (50&deg;F).</div><br/> <div class="paragraph">These limits distinguish it, respectively, from [[tropical rainy climates]], [[snow forest climates]],  and [[tundra climates]]. It is separated from the [[dry climates]] by a function of annual [[temperature]]  and [[precipitation]]. In C. W. Thornthwaite's 1931 classifications, the humid or moist subhumid  and [[mesothermal climates]] would very closely correspond to the above. <br/>''See'' formulas under [[steppe  climate]].</div><br/> </div><div class="reference">K&ouml;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 09:14, 28 March 2024

One of the major categories (the C climate) in W. Köppen's 1936 climatic classification. These climates have a coldest-month mean temperature of less than 18°C (64.4°F) and greater than -3°C (26.6°F), with a warmest-month mean temperature of more than 10°C (50°F).
These limits distinguish it, respectively, from tropical rainy climates, snow forest climates, and tundra climates. It is separated from the dry climates by a function of annual temperature and precipitation. In C. W. Thornthwaite's 1931 classifications, the humid or moist subhumid and mesothermal climates would very closely correspond to the above.
See formulas under steppe climate.
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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