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Differential analysis - Revision history
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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;">TermSearch}}</del></div></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;">|Num</ins>=<ins style="font-weight: bold; text-decoration: none;">1</ins></div></td></tr>
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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 class</del>=<del style="font-weight: bold; text-decoration: none;">"termentry"></del></div></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>[[synoptic analysis|Synoptic analysis]] of change charts or of vertical differential charts (such as [[thickness charts]]) obtained by the graphical or numerical subtraction of the patterns of some meteorological [[variable]] at two times or two levels.<br/> Spatial differential analysis from one surface to another in the vertical is useful because of its relation to [[hydrostatics]]: Differential analysis of [[pressure]] at low levels gives the mean [[isopycnic lines]] for the layer; differential analysis of [[temperature]] and [[potential temperature]] at two levels approximates the mean [[stability]] for the layer; and differential analysis of the topographies of two different [[isobaric surfaces]] gives the pattern of [[thickness]] or mean virtual [[isotherms]] for the layer.<br/> Saucier, W. J. 1955. Principles of Meteorological Analysis. 136&ndash;137. </div></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="term"></del></div></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>}}</div></td></tr>
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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> </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"></del>[[synoptic analysis|Synoptic analysis]] of change charts or of vertical differential charts (such as [[thickness charts]]) obtained by the graphical or numerical subtraction of the patterns of some meteorological [[variable]] at two times or two levels.<del style="font-weight: bold; text-decoration: none;"></div></del><br/<del style="font-weight: bold; text-decoration: none;">> <div class="paragraph"</del>>Spatial differential analysis from one surface to another in the vertical is useful because of its relation to [[hydrostatics]]: Differential analysis of [[pressure]] at low levels gives the mean [[isopycnic lines]] for the layer; differential analysis of [[temperature]] and [[potential temperature]] at two levels approximates the mean [[stability]] for the layer; and differential analysis of the topographies of two different [[isobaric surfaces]] gives the pattern of [[thickness]] or mean virtual [[isotherms]] for the layer.<del style="font-weight: bold; text-decoration: none;"></div></del><br/<del style="font-weight: bold; text-decoration: none;">> </div><div class="reference"</del>>Saucier, W. J. 1955. Principles of Meteorological Analysis. 136&ndash;137. <del style="font-weight: bold; text-decoration: none;"></div><br/> </del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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WikiTeq
https://glossary.ametsoc.org/w/index.php?title=Differential_analysis&diff=16388&oldid=prev
Unknown user at 23:47, 25 April 2012
2012-04-25T23:47:51Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:47, 25 April 2012</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></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><div class="definition"><div class="short_definition">[[Synoptic analysis]] of change charts or of vertical differential charts (such as [[thickness charts]]) obtained by the graphical or numerical subtraction of the patterns of some meteorological [[variable]] at two times or two levels.</div><br/> <div class="paragraph">Spatial differential analysis from one surface to another in the vertical is useful because of its relation to [[hydrostatics]]: Differential analysis of [[pressure]] at low levels gives the mean [[isopycnic lines]] for the layer; differential analysis of [[temperature]] and [[potential temperature]] at two levels approximates the mean [[stability]] for the layer; and differential analysis of the topographies of two different [[isobaric surfaces]] gives the pattern of [[thickness]] or mean virtual [[isotherms]] for the layer.</div><br/> </div><div class="reference">Saucier, W. J. 1955. Principles of Meteorological Analysis. 136&ndash;137. </div><br/> </div></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><div class="definition"><div class="short_definition">[[<ins style="font-weight: bold; text-decoration: none;">synoptic analysis|</ins>Synoptic analysis]] of change charts or of vertical differential charts (such as [[thickness charts]]) obtained by the graphical or numerical subtraction of the patterns of some meteorological [[variable]] at two times or two levels.</div><br/> <div class="paragraph">Spatial differential analysis from one surface to another in the vertical is useful because of its relation to [[hydrostatics]]: Differential analysis of [[pressure]] at low levels gives the mean [[isopycnic lines]] for the layer; differential analysis of [[temperature]] and [[potential temperature]] at two levels approximates the mean [[stability]] for the layer; and differential analysis of the topographies of two different [[isobaric surfaces]] gives the pattern of [[thickness]] or mean virtual [[isotherms]] for the layer.</div><br/> </div><div class="reference">Saucier, W. J. 1955. Principles of Meteorological Analysis. 136&ndash;137. </div><br/> </div></td></tr>
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Unknown user
https://glossary.ametsoc.org/w/index.php?title=Differential_analysis&diff=16387&oldid=prev
Unknown user: Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == differential analysis == </div> <div class="definition"><div class="short_definition">[[Syn..."
2012-01-27T00:50:59Z
<p>Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == differential analysis == </div> <div class="definition"><div class="short_definition">[[Syn..."</p>
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== differential analysis ==<br />
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<div class="definition"><div class="short_definition">[[Synoptic analysis]] of change charts or of vertical differential charts (such as [[thickness charts]]) obtained by the graphical or numerical subtraction of the patterns of some meteorological [[variable]] at two times or two levels.</div><br/> <div class="paragraph">Spatial differential analysis from one surface to another in the vertical is useful because of its relation to [[hydrostatics]]: Differential analysis of [[pressure]] at low levels gives the mean [[isopycnic lines]] for the layer; differential analysis of [[temperature]] and [[potential temperature]] at two levels approximates the mean [[stability]] for the layer; and differential analysis of the topographies of two different [[isobaric surfaces]] gives the pattern of [[thickness]] or mean virtual [[isotherms]] for the layer.</div><br/> </div><div class="reference">Saucier, W. J. 1955. Principles of Meteorological Analysis. 136&ndash;137. </div><br/> <br />
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Unknown user