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	<id>https://wiki.icingcentre.eu/index.php?action=history&amp;feed=atom&amp;title=Wind</id>
	<title>Wind - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://wiki.icingcentre.eu/index.php?action=history&amp;feed=atom&amp;title=Wind"/>
	<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;action=history"/>
	<updated>2026-06-26T00:12:16Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.44.5</generator>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=937&amp;oldid=prev</id>
		<title>Novia at 10:59, 15 February 2022</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=937&amp;oldid=prev"/>
		<updated>2022-02-15T10:59:57Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&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 13:59, 15 February 2022&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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;[[File:&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Windspeed graph&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;jpg&lt;/del&gt;|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The effect of wind speed and temperature in the formation of different incloud ice types.|452x452px&lt;/del&gt;]]&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;[[File:&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Wind3&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;png&lt;/ins&gt;|thumb|&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;391x391px|The effect of wind speed and temperature in the formation of different incloud ice types (soft rime, hard rime, glaze). &lt;/ins&gt;&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&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;&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature. Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature. Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=850&amp;oldid=prev</id>
		<title>Novia at 08:11, 11 February 2022</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=850&amp;oldid=prev"/>
		<updated>2022-02-11T08:11:46Z</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 11:11, 11 February 2022&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-l7&quot;&gt;Line 7:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 7:&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;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; 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;/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;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;== References ==&lt;/ins&gt;&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;&amp;lt;references /&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;&amp;lt;references /&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=775&amp;oldid=prev</id>
		<title>Novia at 08:39, 2 February 2022</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=775&amp;oldid=prev"/>
		<updated>2022-02-02T08:39:17Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&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 11:39, 2 February 2022&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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;537x537px&lt;/del&gt;]]&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;452x452px&lt;/ins&gt;]]&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature. Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature. Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=586&amp;oldid=prev</id>
		<title>Novia at 10:32, 28 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=586&amp;oldid=prev"/>
		<updated>2021-12-28T10:32:58Z</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;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:32, 28 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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|537x537px]]&amp;#039;&amp;#039;&amp;#039;Wind&amp;#039;&amp;#039;&amp;#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|537x537px]]&amp;#039;&amp;#039;&amp;#039;Wind&amp;#039;&amp;#039;&amp;#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what [[ice type]] is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;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; 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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature. Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&quot;:0&quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&quot;:0&quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&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;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;&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://www.semanticscholar.org/paper/Properties-of-icephobic-surfaces-in-different-icing-Stenroos/d40a044131114b37dbdb41d793ffc849a765a6d8&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;&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://www.semanticscholar.org/paper/Properties-of-icephobic-surfaces-in-different-icing-Stenroos/d40a044131114b37dbdb41d793ffc849a765a6d8&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=554&amp;oldid=prev</id>
		<title>Novia at 10:51, 21 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=554&amp;oldid=prev"/>
		<updated>2021-12-21T10:51:53Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:51, 21 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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|537x537px]]&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of ice &lt;/del&gt;is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|537x537px]]&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[ice &lt;/ins&gt;type&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;is formed. Wind speed changes the impact velocity, that influences the ice type.  &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;The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;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;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=553&amp;oldid=prev</id>
		<title>Novia at 10:49, 21 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=553&amp;oldid=prev"/>
		<updated>2021-12-21T10:49:28Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:49, 21 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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.|537x537px]]&lt;/ins&gt;&#039;&#039;&#039;Wind&#039;&#039;&#039; is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;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;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=545&amp;oldid=prev</id>
		<title>Novia at 10:50, 17 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=545&amp;oldid=prev"/>
		<updated>2021-12-17T10:50:02Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:50, 17 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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;Wind is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;&#039;&#039;&lt;/ins&gt;Wind&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;&#039;&#039; &lt;/ins&gt;is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=538&amp;oldid=prev</id>
		<title>Novia at 10:36, 17 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=538&amp;oldid=prev"/>
		<updated>2021-12-17T10:36:47Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:36, 17 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-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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;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; 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;&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;&lt;/del&gt;&amp;lt;ref name=&quot;:0&quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://www.semanticscholar.org/paper/Properties-of-icephobic-surfaces-in-different-icing-Stenroos/d40a044131114b37dbdb41d793ffc849a765a6d8&amp;lt;/ref&amp;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;&amp;lt;ref name=&quot;:0&quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://www.semanticscholar.org/paper/Properties-of-icephobic-surfaces-in-different-icing-Stenroos/d40a044131114b37dbdb41d793ffc849a765a6d8&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;/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;/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;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;&amp;lt;references /&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;&amp;lt;references /&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=537&amp;oldid=prev</id>
		<title>Novia at 10:35, 17 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=537&amp;oldid=prev"/>
		<updated>2021-12-17T10:35:43Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:35, 17 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-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&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;Wind is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;Wind is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Stenroos&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;C. (2015) Properties &lt;/del&gt;of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;icephobic surfaces in different icing conditions. https://pdfslide&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;net/download/link/christian-stenroos-properties-of-icephobic-surfaces-in-different-icing-&lt;/del&gt;&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&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;[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ISO-12494&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Atmospheric icing &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;structures, 2001, 56 p&lt;/ins&gt;.&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&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;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 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;&amp;lt;ref&amp;gt;ISO-12494, Atmospheric icing of structures, 2001, 56 p.&amp;lt;/ref&amp;gt;&amp;lt;ref name=&quot;:0&quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://www.semanticscholar.org/paper/Properties-of-icephobic-surfaces-in-different-icing-Stenroos/d40a044131114b37dbdb41d793ffc849a765a6d8&amp;lt;/ref&amp;gt;&lt;/ins&gt;&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;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; 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;&amp;lt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ref name=&quot;:0&quot; &lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://pdfslide.net/download/link/christian-stenroos-properties-of-icephobic-surfaces-in-different-icing-&amp;lt;/ref&lt;/del&gt;&amp;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;&amp;lt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;references &lt;/ins&gt;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
	<entry>
		<id>https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=536&amp;oldid=prev</id>
		<title>Novia: wind new topic</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Wind&amp;diff=536&amp;oldid=prev"/>
		<updated>2021-12-17T10:27:18Z</updated>

		<summary type="html">&lt;p&gt;wind new topic&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;Wind is an important factor in ice formation. The speed and direction of the wind have a great effect on the shape of the icing layer. Wind speed can change what type of ice is formed. Wind speed changes the impact velocity, that influences the ice type. The figure shows how higher wind speeds extend the temperature area for the creation of glaze ice. Wind causes the water droplets to move faster. This prevents them freezing on the surface immediately. This means that glaze can form at a lower temperature.&lt;br /&gt;
[[File:Windspeed graph.jpg|thumb|&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://pdfslide.net/download/link/christian-stenroos-properties-of-icephobic-surfaces-in-different-icing-&amp;lt;/ref&amp;gt;The effect of wind speed and temperature in the formation of different incloud ice types.]]&lt;br /&gt;
Wind speed also has an effect on the icing rate, not just ice type. In a study by K.J. Sanders and B.L. Barjenbruch &amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;Sanders, B. (2016). Analysis of Ice-to-Liquid Ratios during Freezing Rain and the Development of an Ice Accumulation Model. Weather and Forecasting, 31(4), 1041–1060.&amp;lt;/ref&amp;gt;, ice to water ratio was examined in relation to different wind speed. The study has shown that at wind speeds under 1,5 m/s the ice liquid ratio is 1. When wind speed is above 7.65 m/s, ice to water ratio was 1.9. The study shows a clear increase of icing rate with the increase of wind speed.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&amp;lt;ref&amp;gt;Stenroos, C. (2015) Properties of icephobic surfaces in different icing conditions. https://pdfslide.net/download/link/christian-stenroos-properties-of-icephobic-surfaces-in-different-icing-&amp;lt;/ref&amp;gt;&lt;/div&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
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