https://glossary.ametsoc.org/w/index.php?title=Dry_climates&feed=atom&action=history
Dry climates - Revision history
2024-03-28T11:56:02Z
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https://glossary.ametsoc.org/w/index.php?title=Dry_climates&diff=30470&oldid=prev
WikiTeq: Rewrite with Template:Term and clean up
2024-03-27T20:45:04Z
<p>Rewrite with <a href="/wiki/Template:Term" title="Template:Term">Template:Term</a> and clean up</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:45, 27 March 2024</td>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"> </div></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">#<div class="definition"><div class="short_definition">In W. K&#x000f6;ppen's 1918 [[climatic classification]], the major category (B climates), which includes [[steppe climate]] and [[desert climate]].</div><br/> <div class="paragraph">These climates, unlike the others in his work, are defined strictly by the amount of annual [[precipitation]] as a function of seasonal distribution and of annual [[temperature]] (see formulas under [[steppe climate]]). In contrast are the [[rainy climates]].</div><br/> </div></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">#<div class="definition"><div class="short_definition">In C. W. Thornthwaite's 1948 [[climatic classification]], any [[climate]] type in which the seasonal [[water surplus]] does not counteract seasonal water deficiency; thus it has a [[moisture index]] of less than zero.</div><br/> <div class="paragraph">These types include the [[dry subhumid]], [[semiarid]], and [[arid climates]]. In contrast are the [[moist climates]]. The dry climates are subdivided further according to values of [[humidity index]] into the following: little or no water surplus; moderate winter water surplus; moderate summer water surplus; large winter water surplus; large summer water surplus.</div><br/> </div><div class="reference">K&#x000f6;ppen, W. P. 1918. Klassification der Klimate nach Temperatur, Niederschlag und Jahreslauf. Petermanns Geog. Mitt.. 64. 193&ndash;203; 243&ndash;248. </div><br/> <div class="reference">Thornthwaite, C. W. 1948. An approach toward a rational classification of climate. Geogr. Rev.. 38. 55&ndash;94. </div><br/> </del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">|Meaning=#In W. K&#x000f6;ppen's 1918 </ins>[[<ins style="font-weight: bold; text-decoration: none;">climatic classification]], the major category (B climates), which includes [[steppe climate]] and [[desert climate]].</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">|Explanation=These climates, unlike the others in his work, are defined strictly by the amount of annual [[precipitation]] as a function of seasonal distribution and of annual [[temperature]] (see formulas under [[steppe climate]]). In contrast are the [[rainy climates]].<br/> </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">#In C. W. Thornthwaite's 1948 [[climatic classification]], any [[climate]] type in which the seasonal [[water surplus]] does not counteract seasonal water deficiency; thus it has a [[moisture index]] of less than zero.<br/> These types include the [[dry subhumid]], [[semiarid]], and [[arid climates]]. In contrast are the [[moist climates]]. The dry climates are subdivided further according to values of [[humidity index</ins>]] <ins style="font-weight: bold; text-decoration: none;">into the following: little or no water surplus; moderate winter water surplus; moderate summer water surplus; large winter water surplus; large summer water surplus.<br/> K&#x000f6;ppen, W. P. 1918. Klassification der Klimate nach Temperatur, Niederschlag und Jahreslauf. Petermanns Geog. Mitt.. 64. 193&ndash;203; 243&ndash;248. <br/> Thornthwaite, C. W. 1948. An approach toward a rational classification of climate. Geogr. Rev.. 38. 55&ndash;94. </ins></div></td></tr>
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WikiTeq
https://glossary.ametsoc.org/w/index.php?title=Dry_climates&diff=17003&oldid=prev
Unknown user: Redirected page to Dry climate
2012-04-26T00:09:29Z
<p>Redirected page to <a href="/wiki/Dry_climate" title="Dry climate">Dry climate</a></p>
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#REDIRECT [[dry climate]]<br />
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#<div class="definition"><div class="short_definition">In W. K&#x000f6;ppen's 1918 [[climatic classification]], the major category (B climates), which includes [[steppe climate]] and [[desert climate]].</div><br/> <div class="paragraph">These climates, unlike the others in his work, are defined strictly by the amount of annual [[precipitation]] as a function of seasonal distribution and of annual [[temperature]] (see formulas under [[steppe climate]]). In contrast are the [[rainy climates]].</div><br/> </div><br />
#<div class="definition"><div class="short_definition">In C. W. Thornthwaite's 1948 [[climatic classification]], any [[climate]] type in which the seasonal [[water surplus]] does not counteract seasonal water deficiency; thus it has a [[moisture index]] of less than zero.</div><br/> <div class="paragraph">These types include the [[dry subhumid]], [[semiarid]], and [[arid climates]]. In contrast are the [[moist climates]]. The dry climates are subdivided further according to values of [[humidity index]] into the following: little or no water surplus; moderate winter water surplus; moderate summer water surplus; large winter water surplus; large summer water surplus.</div><br/> </div><div class="reference">K&#x000f6;ppen, W. P. 1918. Klassification der Klimate nach Temperatur, Niederschlag und Jahreslauf. Petermanns Geog. Mitt.. 64. 193&ndash;203; 243&ndash;248. </div><br/> <div class="reference">Thornthwaite, C. W. 1948. An approach toward a rational classification of climate. Geogr. Rev.. 38. 55&ndash;94. </div><br/> <br />
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Unknown user