Climatic province: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">A region of the earth's surface characterized by an essentially homogeneous [[climate]].</div><br/><div class="paragraph">A. Supan (1884) defined 34 different climatic provinces mainly by [[temperature]] and [[rainfall]], partly by [[wind]] and [[orography]]. <br/>''Compare'' [[humidity province]], [[temperature province]].</div><br/> </div><div class="reference">Supan, A. 1884. Grundz& | <div class="definition"><div class="short_definition">A region of the earth's surface characterized by an essentially homogeneous [[climate]].</div><br/><div class="paragraph">A. Supan (1884) defined 34 different climatic provinces mainly by [[temperature]] and [[rainfall]], partly by [[wind]] and [[orography]]. <br/>''Compare'' [[humidity province]], [[temperature province]].</div><br/> </div><div class="reference">Supan, A. 1884. Grundzüge der Physischen Erdkunde. Leipzig, . 129–134. </div><br/> | ||
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Latest revision as of 13:52, 20 February 2012
climatic province
A region of the earth's surface characterized by an essentially homogeneous climate.
A. Supan (1884) defined 34 different climatic provinces mainly by temperature and rainfall, partly by wind and orography.
Compare humidity province, temperature province.
Compare humidity province, temperature province.
Supan, A. 1884. Grundzüge der Physischen Erdkunde. Leipzig, . 129–134.
