“Fire Rainbows” are neither fire, nor rainbows, but are so called because of their brilliant pastel colors and flame like appearance. Technically they are known as circumhorizontal arc - an ice halo formed by hexagonal, plate-shaped ice crystals in high level cirrus clouds. The halo is so large that the arc appears parallel to the horizon, hence the name.
Brightly colored circumhorizontal arc occur mostly during the summer and between particular latitudes. When the sun is very high in the sky, sunlight entering flat, hexagon shaped ice crystals gets split into individual colors just like in a prism. The conditions required to form a “fire rainbow” is very precise – the sun has to be at an elevation of 58° or greater, there must be high altitude cirrus clouds with plate-shaped ice crystals, and sunlight has to enter the ice crystals at a specific angle. This is why circumhorizontal arc is such a rare phenomenon.
A colourful circumhorizon arc spans the sky near Fredericton, New Brunswick, Canada, in 2003.
The position of the observer is also important. Circumhorizontal arcs cannot be seen in locations north of 55°N or south of 55°S. Likewise there are certain times of the year when they are visible. For example, in London, England the sun is only high enough for 140 hours between mid-May and late July. While in Los Angeles, the sun is higher than 58 degrees for 670 hours between late March and late September.
Circumhorizontal arcs should not be confused with Iridescent clouds, which can produce a similar effect. While circumhorizontal arc occur only in cirrus clouds, iridescence often occur in altocumulus, cirrocumulus clouds and lenticular clouds but very rarely in cirrus clouds.
Circumhorizon arcs are so large that sometimes we see only parts of them where they happen to 'light' fragments of cirrus cloud. Ed Johnson (site) captured this one on June 8, 2003 on Mount Baden-Powell, California
Circumhorizon arcs are so huge that their colours sometimes appear to be those of the sky itself rather than an ice crystal halo. In this long-lens shot the halo forms a backdrop to a seemingly tiny aircraft. Picture taken at Pilesgrove, New Jersey in July 22, 2007
This circumhorizon display was photographed through a polarized lens above Dublin, Ohio, in May 2009.
Circumhorizon Arc in Alentejo, Portugal, 2006.
Circumhorizontal arc in Scottsdale, Arizona in 2009
Cirrus fragments lit by a circumhorizon arc, Halifax, Nova Scotia, on 3rd July 2001 with the sun 66° high.
This peculiar 'braided' circumhorizon arc was possibly formed by plate crystals in high cirrus fibratus cloud. Pictures taken at Silver City, New Mexico, USA during August 2004.
Circumhorizontal arc seen over Switzerland in June 2007
Circumhorizon arcs are often seen between lower obscuring clouds. This one was seen in Redding, CA in June 2004.
Circumhorizontal arc in Spokane Valley in June 2006
Circumhorizontal arc seen in Spokane Washington State, in June 3, 2006 when the sun was 64° high
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Brightly colored circumhorizontal arc occur mostly during the summer and between particular latitudes. When the sun is very high in the sky, sunlight entering flat, hexagon shaped ice crystals gets split into individual colors just like in a prism. The conditions required to form a “fire rainbow” is very precise – the sun has to be at an elevation of 58° or greater, there must be high altitude cirrus clouds with plate-shaped ice crystals, and sunlight has to enter the ice crystals at a specific angle. This is why circumhorizontal arc is such a rare phenomenon.
A colourful circumhorizon arc spans the sky near Fredericton, New Brunswick, Canada, in 2003.
The position of the observer is also important. Circumhorizontal arcs cannot be seen in locations north of 55°N or south of 55°S. Likewise there are certain times of the year when they are visible. For example, in London, England the sun is only high enough for 140 hours between mid-May and late July. While in Los Angeles, the sun is higher than 58 degrees for 670 hours between late March and late September.
Circumhorizontal arcs should not be confused with Iridescent clouds, which can produce a similar effect. While circumhorizontal arc occur only in cirrus clouds, iridescence often occur in altocumulus, cirrocumulus clouds and lenticular clouds but very rarely in cirrus clouds.
Circumhorizon arcs are so large that sometimes we see only parts of them where they happen to 'light' fragments of cirrus cloud. Ed Johnson (site) captured this one on June 8, 2003 on Mount Baden-Powell, California
Circumhorizon arcs are so huge that their colours sometimes appear to be those of the sky itself rather than an ice crystal halo. In this long-lens shot the halo forms a backdrop to a seemingly tiny aircraft. Picture taken at Pilesgrove, New Jersey in July 22, 2007
This circumhorizon display was photographed through a polarized lens above Dublin, Ohio, in May 2009.
Circumhorizon Arc in Alentejo, Portugal, 2006.
Circumhorizontal arc in Scottsdale, Arizona in 2009
Cirrus fragments lit by a circumhorizon arc, Halifax, Nova Scotia, on 3rd July 2001 with the sun 66° high.
This peculiar 'braided' circumhorizon arc was possibly formed by plate crystals in high cirrus fibratus cloud. Pictures taken at Silver City, New Mexico, USA during August 2004.
Circumhorizontal arc seen over Switzerland in June 2007
Circumhorizon arcs are often seen between lower obscuring clouds. This one was seen in Redding, CA in June 2004.
Circumhorizontal arc in Spokane Valley in June 2006
Circumhorizontal arc seen in Spokane Washington State, in June 3, 2006 when the sun was 64° high
Source
