<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="en">
	<id>https://wiki.icingcentre.eu/index.php?action=history&amp;feed=atom&amp;title=Turbice_model</id>
	<title>Turbice model - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://wiki.icingcentre.eu/index.php?action=history&amp;feed=atom&amp;title=Turbice_model"/>
	<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Turbice_model&amp;action=history"/>
	<updated>2026-04-21T11:11:21Z</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=Turbice_model&amp;diff=559&amp;oldid=prev</id>
		<title>Novia at 11:46, 21 December 2021</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Turbice_model&amp;diff=559&amp;oldid=prev"/>
		<updated>2021-12-21T11:46:25Z</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 14:46, 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-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;div&gt;In addition, the model considers &amp;#039;&amp;#039;&amp;#039;the surface roughness of ice&amp;#039;&amp;#039;&amp;#039;, which affects the heat transfer from the blade. Ice roughness equation uses meteorological parameters liquid water content, air temperature, free stream velocity and median volume of the droplet. TURBICE accounts for wet icing caused by blade heating and density of accreted ice as well. TURBICE has been tested both in laboratory and in practice. The modelled icing was close to the real results. However, close to 0 degrees Celsius, TURBICE is possibly less accurate.&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;In addition, the model considers &amp;#039;&amp;#039;&amp;#039;the surface roughness of ice&amp;#039;&amp;#039;&amp;#039;, which affects the heat transfer from the blade. Ice roughness equation uses meteorological parameters liquid water content, air temperature, free stream velocity and median volume of the droplet. TURBICE accounts for wet icing caused by blade heating and density of accreted ice as well. TURBICE has been tested both in laboratory and in practice. The modelled icing was close to the real results. However, close to 0 degrees Celsius, TURBICE is possibly less accurate.&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;ref&amp;gt;Makkonen, L. (2001). Modelling and prevention of ice accretion on wind turbines. Wind Engineering, 25(1), 3–21.&amp;lt;/ref&amp;gt; &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;ref&amp;gt;Makkonen, L. (1981). Estimating Intensity of Atmospheric Ice Accretion on Stationary Structures. Journal of Applied Meteorology (1962), 20(5), 595–600.&amp;lt;/ref&amp;gt; &lt;/del&gt;&amp;lt;ref&amp;gt;Thorsson, P. et al. (2015) Modelling atmospheric icing: A comparison between icing calculated with measured meteorological data and NWP data. Cold regions science and technology. [Online] 119124–131.&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&amp;gt;Makkonen, L. (2001). Modelling and prevention of ice accretion on wind turbines. Wind Engineering, 25(1), 3–21.&amp;lt;/ref&amp;gt; &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; &lt;/ins&gt;&amp;lt;ref&amp;gt;Thorsson, P. et al. (2015) Modelling atmospheric icing: A comparison between icing calculated with measured meteorological data and NWP data. Cold regions science and technology. [Online] 119124–131.&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=Turbice_model&amp;diff=558&amp;oldid=prev</id>
		<title>Novia: Created page with &quot;File:Turbice.jpg|thumb|500x500px|TURBICE simulation results for ice shapes in different air temperatures. The modeled temperatures are a) -27,8ºC b) -19,8ºC c) -13,9ºC d)...&quot;</title>
		<link rel="alternate" type="text/html" href="https://wiki.icingcentre.eu/index.php?title=Turbice_model&amp;diff=558&amp;oldid=prev"/>
		<updated>2021-12-21T11:26:45Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;File:Turbice.jpg|thumb|500x500px|TURBICE simulation results for ice shapes in different air temperatures. The modeled temperatures are a) -27,8ºC b) -19,8ºC c) -13,9ºC d)...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Turbice.jpg|thumb|500x500px|TURBICE simulation results for ice shapes in different air temperatures. The modeled temperatures are a) -27,8ºC b) -19,8ºC c) -13,9ºC d) -6,7ºC e) -3,9ºC f) - 2,8ºC.&amp;lt;ref&amp;gt;Makkonen, L. (1981). Estimating Intensity of Atmospheric Ice Accretion on Stationary Structures. Journal of Applied Meteorology (1962), 20(5), 595–600.&amp;lt;/ref&amp;gt;]]&lt;br /&gt;
The TURBICE model is a commonly used icing model for icing on wind turbine blades developed by Makkonen et al.&lt;br /&gt;
&lt;br /&gt;
Both glaze and rime can be modeled, and the model can include blades with anti-icing systems, like heated blades. The model can show the shape and size of accreted ice and includes the effect of liquid water on the blades. TURBICE model has equations to account for the air flow and droplet trajectories.&lt;br /&gt;
&lt;br /&gt;
The figure shows how TURBICE model can be used to estimate the shape of the ice. Blue line on the graph is the ice formation, and the black line is the turbine blade.&lt;br /&gt;
&lt;br /&gt;
In addition, the model considers &amp;#039;&amp;#039;&amp;#039;the surface roughness of ice&amp;#039;&amp;#039;&amp;#039;, which affects the heat transfer from the blade. Ice roughness equation uses meteorological parameters liquid water content, air temperature, free stream velocity and median volume of the droplet. TURBICE accounts for wet icing caused by blade heating and density of accreted ice as well. TURBICE has been tested both in laboratory and in practice. The modelled icing was close to the real results. However, close to 0 degrees Celsius, TURBICE is possibly less accurate.&lt;br /&gt;
&lt;br /&gt;
&amp;lt;ref&amp;gt;Makkonen, L. (2001). Modelling and prevention of ice accretion on wind turbines. Wind Engineering, 25(1), 3–21.&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Makkonen, L. (1981). Estimating Intensity of Atmospheric Ice Accretion on Stationary Structures. Journal of Applied Meteorology (1962), 20(5), 595–600.&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Thorsson, P. et al. (2015) Modelling atmospheric icing: A comparison between icing calculated with measured meteorological data and NWP data. Cold regions science and technology. [Online] 119124–131.&amp;lt;/ref&amp;gt;&lt;/div&gt;</summary>
		<author><name>Novia</name></author>
	</entry>
</feed>