Fire Rainbow | eAmazings

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Thursday, 09 February 2012

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Amazing & Intresting

Fire Rainbow

Wednesday, 04 August 2010 00:00

The phenomenon known as a “fire rainbow” does exist. Here, read the science behind it and marvel at some amazing photography of this rare beauty, the Circumhorizon Arc, known to its friends as a CHA.

If you are very lucky you may see a fire rainbow once or twice in your life. It sounds like it could be one of a series of children’s books - “Harry Potter and the Fire Rainbow” has a certain ring to it, but this phenomenon is not fiction. If you are in the right place and at the right time then a fire rainbow is something that you will remember witnessing forever.

To name it properly, a fire rainbow is a circumhorizontal arc. It is also known as a circumhorizon arc but whichever you chose, scientists (and aficionados) call it a CHA. It is given its name because it looks as if a rainbow has spontaneously combusted as it made its way across the sky. It could even be suspected, perhaps, that some malign fairy or goblin has blown the rainbow up to stop some errant human discovering that elusive pot of gold at its end!

The real explanation behind a fire rainbow lies more in science text books than in a Brothers Grimm tale. A CHA is a kind of halo - which is an optical phenomenon. These appear around the moon - or in this case the Sun. You have probably seen a halo yourself around a strong light source - take a look at street lights in the fog for example.

Fire Rainbow

Although there are many different types of optical halos, a CHA is caused by the refraction though ice crystals in cirrus clouds of light from the sun. Refraction happens when the speed of light is reduced inside a particular medium. This particular refraction happens when light goes from air without cloud to air containing cloud. In this case it is vital that the cloud is cirrus in shape.

Fire Rainbow

A cirrus cloud is one of those thin, wispy ones, often with tufts sticking out like disheveled hair! They can be huge - covering so much of the sky that you cannot see where one ends and another begins. When they are a massive sheet they are called cirrostratus. They are formed at enormous heights - over eight thousand meters. There is very little moisture at those heights and that’s why they are so skinny!

So, what happens when light hits a cirrus cloud and what special conditions are needed to form a fire rainbow? The refraction of the light causes it to separate from its “white” form to its different components (which people call wavelengths). The person on the street would say that the light is bent out of shape and split up in to all the different colors that make it up. In other words, a rainbow - or in our case, a fire rainbow!

So, why don’t you see fire rainbows as often as (its now more mundane!) cousin, the rainbow? For a start the sun has to be at least fifty eight degrees above the horizon for one to occur - and you have to be lucky enough to have cirrus clouds around at the same time! Because of the necessary height of the sun you will not see a fire rainbow north of fifty five degrees - and likewise further south of the magic fifty five degrees. You may occasionally see one if you are high up on a mountain further south or north, but it is not likely!

There is more! The ice crystals in the cirrus cloud have to be horizontal to refract the sun. If they are then the arc is formed. Ice crystals have six sides, meaning that they are hexagonal. The light goes in through one of the side faces of the crystal. Then it is refracted and it leaves through the bottom horizontal face. Below is my rather poor attempt to reproduce the process in PowerPoint!

It is vital that the crystal is aligned just so as otherwise the light will not separate in to the rainbow like colors you expect. If the alignment is correct then the whole cirrus cloud will “explode” in to a flaming, fire rainbow! The sight is almost as if someone has sprayed the sky with gasoline, thrown a lit match at it and then leant back, arms folded, to take in their handiwork!