https://wiki.icingcentre.eu/index.php?action=history&feed=atom&title=Icing
Icing - Revision history
2026-06-10T09:35:32Z
Revision history for this page on the wiki
MediaWiki 1.44.5
https://wiki.icingcentre.eu/index.php?title=Icing&diff=957&oldid=prev
Novia at 12:04, 15 February 2022
2022-02-15T12:04:58Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 15:04, 15 February 2022</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;"><div>[[In-cloud icing]] happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have [[Supercooled water|super-cooled droplets]] in them, which freeze upon contact with the surface.</div></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;"><div>[[In-cloud icing]] happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have [[Supercooled water|super-cooled droplets]] in them, which freeze upon contact with the surface.</div></td></tr>
<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>[[Precipitation icing]] happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with [[Freezing rain|freezing rain.]] </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>[[Precipitation icing]] happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with [[Freezing rain|freezing rain.]]</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> </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;">[[File:Tree branch after ice storm..jpg|thumb|387x387px|Tree branch after ice storm. <ref>J. Carmichael. Wikimedia commons. Public domain. 2009. Tree branch after ice storm.JPG</ref>]]</ins></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><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></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><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref> </div></td></tr>
<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"></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;"><div>Most apparent effect on icing is temperature, which has to be under zero degrees Celsius for water to freeze. Second thing needed for ice is water, so there needs to be enough humidity, for example rain, for ice to form. Snow can also form ice, especially when combined with liquid water. '''[https://wiki.icingcentre.eu/index.php/Wind Wind]''' is also an important factor in ice formation. </div></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;"><div>Most apparent effect on icing is temperature, which has to be under zero degrees Celsius for water to freeze. Second thing needed for ice is water, so there needs to be enough humidity, for example rain, for ice to form. Snow can also form ice, especially when combined with liquid water. '''[https://wiki.icingcentre.eu/index.php/Wind Wind]''' is also an important factor in ice formation. </div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=933&oldid=prev
Novia at 10:51, 15 February 2022
2022-02-15T10:51:12Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:51, 15 February 2022</td>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[File:<del style="font-weight: bold; text-decoration: none;">Icing6</del>.png|thumb|<del style="font-weight: bold; text-decoration: none;">477x477px</del>|<del style="font-weight: bold; text-decoration: none;">Atmospheric </del>icing]]</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>[[File:<ins style="font-weight: bold; text-decoration: none;">Icing9</ins>.png|thumb|<ins style="font-weight: bold; text-decoration: none;">386x386px</ins>|<ins style="font-weight: bold; text-decoration: none;">Classification of atmospheric </ins>icing<ins style="font-weight: bold; text-decoration: none;">. </ins>]]</div></td></tr>
<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;"><div>'''Icing''' in nature can happen mainly in two different ways: by [[in-cloud icing]] or [[Precipitation icing|precipitation icing.]] </div></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;"><div>'''Icing''' in nature can happen mainly in two different ways: by [[in-cloud icing]] or [[Precipitation icing|precipitation icing.]] </div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=921&oldid=prev
Novia at 12:17, 11 February 2022
2022-02-11T12:17:07Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 15:17, 11 February 2022</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;"><div>'''Icing''' in nature can happen mainly in two different ways: by [[in-cloud icing]] or [[Precipitation icing|precipitation icing.]] </div></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;"><div>'''Icing''' in nature can happen mainly in two different ways: by [[in-cloud icing]] or [[Precipitation icing|precipitation icing.]] </div></td></tr>
<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>In-cloud icing happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have [[Supercooled water|super-cooled droplets]] in them, which freeze upon contact with the surface.</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;">[[</ins>In-cloud icing<ins style="font-weight: bold; text-decoration: none;">]] </ins>happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have [[Supercooled water|super-cooled droplets]] in them, which freeze upon contact with the surface.</div></td></tr>
<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>Precipitation icing happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with [[Freezing rain|freezing rain.]] </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;">[[</ins>Precipitation icing<ins style="font-weight: bold; text-decoration: none;">]] </ins>happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with [[Freezing rain|freezing rain.]] </div></td></tr>
<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"></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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></td></tr>
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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"></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">More on this topic: [[Atmospheric Icing|atmospheric icing]]</ins></div></td></tr>
<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"></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;"><div>== References ==</div></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;"><div>== References ==</div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=919&oldid=prev
Novia at 12:15, 11 February 2022
2022-02-11T12:15:18Z
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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>[[File:<del style="font-weight: bold; text-decoration: none;">Atmospheric icing </del>.<del style="font-weight: bold; text-decoration: none;">jpg</del>|thumb|<del style="font-weight: bold; text-decoration: none;">536x536px</del>|<del style="font-weight: bold; text-decoration: none;">atmospheric </del>icing <del style="font-weight: bold; text-decoration: none;">categories</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>[[File:<ins style="font-weight: bold; text-decoration: none;">Icing6</ins>.<ins style="font-weight: bold; text-decoration: none;">png</ins>|thumb|<ins style="font-weight: bold; text-decoration: none;">477x477px</ins>|<ins style="font-weight: bold; text-decoration: none;">Atmospheric </ins>icing]]</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>'''Icing''' in nature can happen mainly in two different ways: by in-cloud icing or precipitation icing.</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>'''Icing''' in nature can happen mainly in two different ways: by <ins style="font-weight: bold; text-decoration: none;">[[</ins>in-cloud icing<ins style="font-weight: bold; text-decoration: none;">]] </ins>or <ins style="font-weight: bold; text-decoration: none;">[[Precipitation icing|</ins>precipitation icing.<ins style="font-weight: bold; text-decoration: none;">]] </ins></div></td></tr>
<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>In-cloud icing happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have super-cooled droplets in them, which freeze upon contact with the surface.</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>In-cloud icing happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have <ins style="font-weight: bold; text-decoration: none;">[[Supercooled water|</ins>super-cooled droplets<ins style="font-weight: bold; text-decoration: none;">]] </ins>in them, which freeze upon contact with the surface.</div></td></tr>
<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>Precipitation icing happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with freezing rain. </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>Precipitation icing happens when a liquid water drops fall on a surface and then freeze. Precipitation icing happens during rain or snowfall, when the precipitation freezes as it contacts the surface. If temperature is between 0 and 3 degrees Celsius, then the falling snowflakes contain liquid water, which enables them to bond weakly with each other. After this, the bond strengthens when temperature drops below zero degrees Celsius. Rain causes precipitation icing when the temperature is below zero. This happens for example with <ins style="font-weight: bold; text-decoration: none;">[[Freezing rain|</ins>freezing rain.<ins style="font-weight: bold; text-decoration: none;">]] </ins></div></td></tr>
<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"></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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=915&oldid=prev
Novia at 11:51, 11 February 2022
2022-02-11T11:51:13Z
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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;"><div>'''Icing''' in nature can happen mainly in two different ways: by in-cloud icing or precipitation icing.</div></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;"><div>'''Icing''' in nature can happen mainly in two different ways: by in-cloud icing or precipitation icing.</div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=846&oldid=prev
Novia at 08:07, 11 February 2022
2022-02-11T08:07:01Z
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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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></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>References</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;">== </ins>References <ins style="font-weight: bold; text-decoration: none;">==</ins></div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=755&oldid=prev
Novia at 11:19, 1 February 2022
2022-02-01T11:19:01Z
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=754&oldid=prev
Novia at 11:18, 1 February 2022
2022-02-01T11:18:13Z
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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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=544&oldid=prev
Novia at 10:49, 17 December 2021
2021-12-17T10:49:46Z
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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>Icing in nature can happen mainly in two different ways: by in-cloud icing or precipitation icing.</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;">'''</ins>Icing<ins style="font-weight: bold; text-decoration: none;">''' </ins>in nature can happen mainly in two different ways: by in-cloud icing or precipitation icing.</div></td></tr>
<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"></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;"><div>In-cloud icing happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have super-cooled droplets in them, which freeze upon contact with the surface.</div></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;"><div>In-cloud icing happens when water freezes from a cloud or fog. In-cloud icing happens when there are clouds or fog, that is below zero degrees. These clouds have super-cooled droplets in them, which freeze upon contact with the surface.</div></td></tr>
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Novia
https://wiki.icingcentre.eu/index.php?title=Icing&diff=539&oldid=prev
Novia at 10:38, 17 December 2021
2021-12-17T10:38:56Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:38, 17 December 2021</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l7">Line 7:</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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></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;"><div><ref>Jin, J. Y. (2021) Study of Atmospheric Ice Accretion on Wind Turbine Blades. UiT Norges arktiske universitet. Online. https://munin.uit.no/handle/10037/22115</ref> <ref name=":0">THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT, The weather prediction, webpage, available (accessed 29.2.2021): <nowiki>http://www.theweatherprediction.com/habyhints/210/</nowiki></ref> <ref>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.</ref></div></td></tr>
<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>Most apparent effect on icing is temperature, which has to be under zero degrees Celsius for water to freeze. Second thing needed for ice is water, so there needs to be enough humidity, for example rain, for ice to form. Snow can also form ice, especially when combined with liquid water. '''Wind''' is also an important factor in ice formation. </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>Most apparent effect on icing is temperature, which has to be under zero degrees Celsius for water to freeze. Second thing needed for ice is water, so there needs to be enough humidity, for example rain, for ice to form. Snow can also form ice, especially when combined with liquid water. '''<ins style="font-weight: bold; text-decoration: none;">[https://wiki.icingcentre.eu/index.php/</ins>Wind <ins style="font-weight: bold; text-decoration: none;">Wind]</ins>''' is also an important factor in ice formation. </div></td></tr>
<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"></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></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;"><div><ref name=":0" /> <ref>Ingvaldsen, K. (2017) Atmospheric icing in a changing climate: Impact of higher boundary temperatures on simulations of atmospheric ice accretion on structures during the 2015-2016 icing winter in West-Norway.</ref></div></td></tr>
<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;"><div><references /></div></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;"><div><references /></div></td></tr>
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Novia