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	<id>http://atomix.app.uib.no/index.php?action=history&amp;feed=atom&amp;title=Taylor%27s_Frozen_Turbulence</id>
	<title>Taylor&#039;s Frozen Turbulence - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://atomix.app.uib.no/index.php?action=history&amp;feed=atom&amp;title=Taylor%27s_Frozen_Turbulence"/>
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	<updated>2026-04-28T21:13:54Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.44.2</generator>
	<entry>
		<id>http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=2893&amp;oldid=prev</id>
		<title>CynthiaBluteau at 20:00, 1 December 2021</title>
		<link rel="alternate" type="text/html" href="http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=2893&amp;oldid=prev"/>
		<updated>2021-12-01T20:00:39Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 20:00, 1 December 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l8&quot;&gt;Line 8:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 8:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;As an instrument measures the fluctuations of a variable such as velocity, shear, or temperature with a sensor at one location for a period of time the effect of eddies is observed as they drift by the sensor.  However, the eddies could be changing size and shape as they drift by the sensor.  Solviev and Lukas reduce the practical suitability of any situation to requirement that the fluctuations are within 10% of its mean speed past the sensor&amp;lt;ref&amp;gt;Soloviev, A. and Lukas, R., 2003. Observation of wave-enhanced turbulence in the near-surface layer of the ocean during TOGA COARE. Deep Sea Research Part I: Oceanographic Research Papers, 50(3), pp.371-395. doi:10.1016/S0967-0637(03)00004-9 &amp;lt;/ref&amp;gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;As an instrument measures the fluctuations of a variable such as velocity, shear, or temperature with a sensor at one location for a period of time the effect of eddies is observed as they drift by the sensor.  However, the eddies could be changing size and shape as they drift by the sensor.  Solviev and Lukas reduce the practical suitability of any situation to requirement that the fluctuations are within 10% of its mean speed past the sensor&amp;lt;ref&amp;gt;Soloviev, A. and Lukas, R., 2003. Observation of wave-enhanced turbulence in the near-surface layer of the ocean during TOGA COARE. Deep Sea Research Part I: Oceanographic Research Papers, 50(3), pp.371-395. doi:10.1016/S0967-0637(03)00004-9 &amp;lt;/ref&amp;gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;==Notes==&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>CynthiaBluteau</name></author>
	</entry>
	<entry>
		<id>http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=2552&amp;oldid=prev</id>
		<title>CraigStevens: made a start... but will look for more</title>
		<link rel="alternate" type="text/html" href="http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=2552&amp;oldid=prev"/>
		<updated>2021-11-22T08:29:11Z</updated>

		<summary type="html">&lt;p&gt;made a start... but will look for more&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 08:29, 22 November 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;|article_type=Concept&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;|article_type=Concept&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Provide &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;original citation &lt;/del&gt;of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Taylor&#039;s &lt;/del&gt;hypothesis, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;elaborate &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;meaning &lt;/del&gt;of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&quot;properties&quot;&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Taylor’s frozen turbulence hypothesis (sometimes &quot;frozen field&quot; or &quot;frozen eddy&quot;)&amp;lt;ref&amp;gt;Taylor GI (1938) The spectrum of turbulence. Proc Roy Soc Lond 164: 476–490 https://doi.org/10.1098/rspa.1938.0032&amp;lt;/ref&amp;gt; is a primary assumption invoked when seeking to quantify turbulence physics using time-resolving sensors&amp;lt;ref&amp;gt;Higgins, C.W., Froidevaux, M., Simeonov, V., Vercauteren, N., Barry, C. and Parlange, M.B., 2012. The effect of scale on &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;applicability &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Taylor’s frozen turbulence &lt;/ins&gt;hypothesis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in the atmospheric boundary layer. Boundary-layer meteorology, 143(2), pp.379-391. https://doi.org/10.1007/s10546-012-9701-1&amp;lt;/ref&amp;gt;.  Thus it is applicable to the shear and velocimeter approaches described here. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As an instrument measures the fluctuations of a variable such as velocity, shear, or temperature with a sensor at one location for a period of time the effect of eddies is observed as they drift by the sensor.  However, the eddies could be changing size and shape as they drift by the sensor.  Solviev and Lukas reduce the practical suitability of any situation to requirement that the fluctuations are within 10% of its mean speed past the sensor&amp;lt;ref&amp;gt;Soloviev&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;A. &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Lukas, R., 2003. Observation of wave-enhanced turbulence in &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near-surface layer &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the ocean during TOGA COARE. Deep Sea Research Part I: Oceanographic Research Papers, 50(3), pp.371-395. doi:10.1016/S0967-0637(03)00004-9 &amp;lt;/ref&amp;gt;&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>CraigStevens</name></author>
	</entry>
	<entry>
		<id>http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=1317&amp;oldid=prev</id>
		<title>CynthiaBluteau: Created page with &quot;{{DefineConcept |description=The turbulence eddies advected past a sensor (or that a sensor is passing through) retain their properties |article_type=Concept }} Provide the or...&quot;</title>
		<link rel="alternate" type="text/html" href="http://atomix.app.uib.no/index.php?title=Taylor%27s_Frozen_Turbulence&amp;diff=1317&amp;oldid=prev"/>
		<updated>2021-10-13T23:31:10Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;{{DefineConcept |description=The turbulence eddies advected past a sensor (or that a sensor is passing through) retain their properties |article_type=Concept }} Provide the or...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{DefineConcept&lt;br /&gt;
|description=The turbulence eddies advected past a sensor (or that a sensor is passing through) retain their properties&lt;br /&gt;
|article_type=Concept&lt;br /&gt;
}}&lt;br /&gt;
Provide the original citation of Taylor&amp;#039;s hypothesis, and elaborate the meaning of &amp;quot;properties&amp;quot;.&lt;/div&gt;</summary>
		<author><name>CynthiaBluteau</name></author>
	</entry>
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