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		<title>Pyro-cumulonimbus plumes - Revision history</title>
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		<title>Designing Buildings at 04:16, 20 September 2022</title>
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				<updated>2022-09-20T04:16:45Z</updated>
		
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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Older revision&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Revision as of 04:16, 20 September 2022&lt;/td&gt;
		&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&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='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;[[File:Forest-Fire.jpg]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;[[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;File:Forest-Fire.jpg|link=&lt;/ins&gt;File:Forest-Fire.jpg]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Pyro-cumulonimbus plumes, often called pyroCb for short or more formally &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a &lt;/del&gt;cumulonimbus flammagenitus &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cloud &lt;/del&gt;(CbFg)&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;. It is a cloud that is &lt;/del&gt;generated by extreme heat &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;being &lt;/del&gt;released at the surface of the earth, such as from a volcanic eruption, or a wild fire, in some cases enhanced by localised industrial combustion emissions. They &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/del&gt;a distinctive grey colour because &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;of the &lt;/del&gt;smoke particles, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;these &lt;/del&gt;lead thunderstorms as water condenses on their surface, and they can rise up high into the upper troposphere or lower stratosphere.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;= Introduction =&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Pyro-cumulonimbus plumes, often called pyroCb for short or more formally&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, &lt;/ins&gt;cumulonimbus flammagenitus &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;clouds &lt;/ins&gt;(CbFg)&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, are clouds &lt;/ins&gt;generated by extreme heat released at the surface of the earth, such as from a volcanic eruption, or a wild fire, in some cases enhanced by localised industrial combustion emissions. They &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;can have &lt;/ins&gt;a distinctive grey colour because smoke particles, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which can &lt;/ins&gt;lead &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;to &lt;/ins&gt;thunderstorms as water condenses on their surface, and they can rise up high into the upper troposphere or lower stratosphere.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Examples =&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Examples =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;One of the earliest photographs a major pyroCb occurred in Hiroshima, some time after the atomic bomb and its infamous atomic cloud &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;struck &lt;/del&gt;in 1945. It was caused by the devastating ground level firestorm that jointly killed over 30% population of the city.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;One of the earliest photographs &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;of &lt;/ins&gt;a major pyroCb occurred in Hiroshima, some time after the atomic bomb and its infamous atomic cloud in 1945. It was caused by the devastating ground level firestorm that jointly killed over 30% &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;of the &lt;/ins&gt;population of the city.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 1991,sometime after the eruption of Mount Pinatubo in the Philippines, volcanic thunderstorms formed near its summit, but also in areas away from the summit, near smaller localised heat sources&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;, these cloud &lt;/del&gt;produced rain or mud fall as it contained &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ashs &lt;/del&gt;from the initial &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;erruption&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 1991, sometime after the eruption of Mount Pinatubo in the Philippines, volcanic thunderstorms formed near its summit, but also in areas away from the summit, near smaller localised heat sources&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;. These clouds &lt;/ins&gt;produced rain or mud fall as it contained &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ashes &lt;/ins&gt;from the initial &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;eruption&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 2003, 2009 and 2019 extreme summer wildfires in Australia created what were reported as fire tornadoes and significant lightening clouds throughout the period when the fires burnt. Similar incidences occurred in the US and Canada and elsewhere in 2020-2022, so much so that pyroCb's are often now referred to more commonly as fireclouds.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 2003, 2009 and 2019 extreme summer wildfires in Australia created what were reported as fire tornadoes and significant lightening clouds throughout the period when the fires burnt. Similar incidences occurred in the US and Canada and elsewhere in 2020-2022, so much so that pyroCb's are often now referred to more commonly as fireclouds.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 15:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 17:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 2021 a a meteorologist at the US Naval Research Laboratory noted about fireclouds that:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;In 2021 a a meteorologist at the US Naval Research Laboratory noted about fireclouds that:&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;“You can think of them as like giant chimneys, funneling smoke that's being released by the fire up into a thunderstorm... this extremely dirty thunderstorm, with all these smoke particles for water to condense on.”.. though, the resulting water droplets don’t tend to get large enough to fall as rain. “But it is a cloud that can produce a lot of lightning,” These clouds can then advance across the landscape, sparking new wildfires as they go. So not only can the blaze propagate itself by flinging embers ahead of the main fire line, it can also produce so much hot, rising smoke that it in essence recruits the atmosphere to light more fires &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;for it. It’s a runaway self-proliferating machine&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;“You can think of them as like giant chimneys, funneling smoke that's being released by the fire up into a thunderstorm... this extremely dirty thunderstorm, with all these smoke particles for water to condense on.”.. though, the resulting water droplets don’t tend to get large enough to fall as rain. “But it is a cloud that can produce a lot of lightning,” These clouds can then advance across the landscape, sparking new wildfires as they go. So not only can the blaze propagate itself by flinging embers ahead of the main fire line, it can also produce so much hot, rising smoke that it in essence recruits the atmosphere to light more fires.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Climate change =&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Climate change =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Fourth National Climate Assessment (NCA4), Climate Science Special Report Volume I noted that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the Climate &lt;/del&gt;change enhances the drying of organic matter in forests (the material that burns and spreads wildfire), and has doubled the number of large fires between 1984 and 2015 in the western United States. The top 10 years with the largest annual acreage burned all occurred since 2004, a period which coincides with many of the warmest years on record across the US and worldwide.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;The &lt;/ins&gt;Fourth National Climate Assessment (NCA4), Climate Science Special Report Volume I noted that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;climate &lt;/ins&gt;change enhances the drying of organic matter in forests (the material that burns and spreads wildfire), and has doubled the number of large fires between 1984 and 2015 in the western United States. The top 10 years with the largest annual acreage burned all occurred since 2004, a period which coincides with many of the warmest years on record across the US and worldwide.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Severe drought, heat and low humidity become more common and extreme as the climate warms, these hot and dry conditions are often referred to as fire weather. Scientists can measure changes in fire weather (temperature, humidity, rainfall and wind) to rate the level of danger of a wildfire striking.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Severe drought, heat and low humidity become more common and extreme as the climate warms, these hot and dry conditions are often referred to as fire weather. Scientists can measure changes in fire weather (temperature, humidity, rainfall and wind) to rate the level of danger of a wildfire striking.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;The Fire Weather Index (FWI) is a meteorologically based index used worldwide to estimate fire danger. It consists of different components that account for the effects of fuel moisture and wind on fire behaviour and spread. The higher the FWI &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is&lt;/del&gt;, the more favourable the meteorological conditions &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;to trigger &lt;/del&gt;a wildfire &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;The Fire Weather Index (FWI) is a meteorologically based index used worldwide to estimate fire danger. It consists of different components that account for the effects of fuel moisture and wind on fire behaviour and spread. The higher the FWI, the more favourable the meteorological conditions &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are for triggering &lt;/ins&gt;a wildfire.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;= External Links =&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[https://climate.copernicus.eu/fire-weather-index https://climate.copernicus.eu/fire-weather-index]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[https://glossary.ametsoc.org/wiki/Welcome https://glossary.ametsoc.org/wiki/Welcome]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[https://www.nature.com/articles/s41612-021-00192-9 https://www.nature.com/articles/s41612-021-00192-9]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;minus;&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/ https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Related articles on Designing Buildings =&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;= Related articles on Designing Buildings =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 48:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 42:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;* Global warming.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;* Global warming.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;* Weather.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;* Weather.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;= External references =&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;* [https://climate.copernicus.eu/fire-weather-index https://climate.copernicus.eu/fire-weather-index]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;* [https://glossary.ametsoc.org/wiki/Welcome https://glossary.ametsoc.org/wiki/Welcome]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;* [https://www.nature.com/articles/s41612-021-00192-9 https://www.nature.com/articles/s41612-021-00192-9]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;* [https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/ https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;[[Category:DCN_Definition]] [[Category:DCN_Research,_Development_and_Innovation]] [[Category:Definitions]] [[Category:Research_/_Innovation]] [[Category:Theory]] [[Category:Standards_/_measurements]] [[Category:Sustainability]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;[[Category:DCN_Definition]] [[Category:DCN_Research,_Development_and_Innovation]] [[Category:Definitions]] [[Category:Research_/_Innovation]] [[Category:Theory]] [[Category:Standards_/_measurements]] [[Category:Sustainability]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Designing Buildings</name></author>	</entry>

	<entry>
		<id>https://www.designingbuildings.co.uk/w/index.php?title=Pyro-cumulonimbus_plumes&amp;diff=238924&amp;oldid=prev</id>
		<title>Editor: Created page with &quot;File:Forest-Fire.jpg  Pyro-cumulonimbus plumes, often called pyroCb for short or more formally a cumulonimbus flammagenitus cloud (CbFg). It is a cloud that is generated by e...&quot;</title>
		<link rel="alternate" type="text/html" href="https://www.designingbuildings.co.uk/w/index.php?title=Pyro-cumulonimbus_plumes&amp;diff=238924&amp;oldid=prev"/>
				<updated>2022-09-14T04:57:31Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;&lt;a href=&quot;/wiki/File:Forest-Fire.jpg&quot; title=&quot;File:Forest-Fire.jpg&quot;&gt;File:Forest-Fire.jpg&lt;/a&gt;  Pyro-cumulonimbus plumes, often called pyroCb for short or more formally a cumulonimbus flammagenitus cloud (CbFg). It is a cloud that is generated by e...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Forest-Fire.jpg]]&lt;br /&gt;
&lt;br /&gt;
Pyro-cumulonimbus plumes, often called pyroCb for short or more formally a cumulonimbus flammagenitus cloud (CbFg). It is a cloud that is generated by extreme heat being released at the surface of the earth, such as from a volcanic eruption, or a wild fire, in some cases enhanced by localised industrial combustion emissions. They are a distinctive grey colour because of the smoke particles, these lead thunderstorms as water condenses on their surface, and they can rise up high into the upper troposphere or lower stratosphere.&lt;br /&gt;
&lt;br /&gt;
= Examples =&lt;br /&gt;
&lt;br /&gt;
One of the earliest photographs a major pyroCb occurred in Hiroshima, some time after the atomic bomb and its infamous atomic cloud struck in 1945. It was caused by the devastating ground level firestorm that jointly killed over 30% population of the city.&lt;br /&gt;
&lt;br /&gt;
In 1991,sometime after the eruption of Mount Pinatubo in the Philippines, volcanic thunderstorms formed near its summit, but also in areas away from the summit, near smaller localised heat sources, these cloud produced rain or mud fall as it contained ashs from the initial erruption.&lt;br /&gt;
&lt;br /&gt;
In 2003, 2009 and 2019 extreme summer wildfires in Australia created what were reported as fire tornadoes and significant lightening clouds throughout the period when the fires burnt. Similar incidences occurred in the US and Canada and elsewhere in 2020-2022, so much so that pyroCb's are often now referred to more commonly as fireclouds.&lt;br /&gt;
&lt;br /&gt;
= Comment =&lt;br /&gt;
&lt;br /&gt;
In 2021 a a meteorologist at the US Naval Research Laboratory noted about fireclouds that:&lt;br /&gt;
&lt;br /&gt;
“You can think of them as like giant chimneys, funneling smoke that's being released by the fire up into a thunderstorm... this extremely dirty thunderstorm, with all these smoke particles for water to condense on.”.. though, the resulting water droplets don’t tend to get large enough to fall as rain. “But it is a cloud that can produce a lot of lightning,” These clouds can then advance across the landscape, sparking new wildfires as they go. So not only can the blaze propagate itself by flinging embers ahead of the main fire line, it can also produce so much hot, rising smoke that it in essence recruits the atmosphere to light more fires for it. It’s a runaway self-proliferating machine.&lt;br /&gt;
&lt;br /&gt;
= Climate change =&lt;br /&gt;
&lt;br /&gt;
Fourth National Climate Assessment (NCA4), Climate Science Special Report Volume I noted that the Climate change enhances the drying of organic matter in forests (the material that burns and spreads wildfire), and has doubled the number of large fires between 1984 and 2015 in the western United States. The top 10 years with the largest annual acreage burned all occurred since 2004, a period which coincides with many of the warmest years on record across the US and worldwide.&lt;br /&gt;
&lt;br /&gt;
Severe drought, heat and low humidity become more common and extreme as the climate warms, these hot and dry conditions are often referred to as fire weather. Scientists can measure changes in fire weather (temperature, humidity, rainfall and wind) to rate the level of danger of a wildfire striking.&lt;br /&gt;
&lt;br /&gt;
The Fire Weather Index (FWI) is a meteorologically based index used worldwide to estimate fire danger. It consists of different components that account for the effects of fuel moisture and wind on fire behaviour and spread. The higher the FWI is, the more favourable the meteorological conditions to trigger a wildfire are.&lt;br /&gt;
&lt;br /&gt;
= External Links =&lt;br /&gt;
&lt;br /&gt;
[https://climate.copernicus.eu/fire-weather-index https://climate.copernicus.eu/fire-weather-index]&lt;br /&gt;
&lt;br /&gt;
[https://glossary.ametsoc.org/wiki/Welcome https://glossary.ametsoc.org/wiki/Welcome]&lt;br /&gt;
&lt;br /&gt;
[https://www.nature.com/articles/s41612-021-00192-9 https://www.nature.com/articles/s41612-021-00192-9]&lt;br /&gt;
&lt;br /&gt;
[https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/ https://www.wired.com/story/oh-good-now-theres-an-outbreak-of-wildfire-thunderclouds/]&lt;br /&gt;
&lt;br /&gt;
= Related articles on Designing Buildings =&lt;br /&gt;
&lt;br /&gt;
* Adaptation.&lt;br /&gt;
* Climate.&lt;br /&gt;
* Climate change.&lt;br /&gt;
* Disaster.&lt;br /&gt;
* Drought.&lt;br /&gt;
* Exceptionally adverse weather.&lt;br /&gt;
* Extreme weather.&lt;br /&gt;
* Fire Weather.&lt;br /&gt;
* Flood.&lt;br /&gt;
* Global warming.&lt;br /&gt;
* Weather.&lt;br /&gt;
&lt;br /&gt;
[[Category:DCN_Definition]] [[Category:DCN_Research,_Development_and_Innovation]] [[Category:Definitions]] [[Category:Research_/_Innovation]] [[Category:Theory]] [[Category:Standards_/_measurements]] [[Category:Sustainability]]&lt;/div&gt;</summary>
		<author><name>Editor</name></author>	</entry>

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