Rare 'rainbow clouds' spotted in UK skies

The Sky News weather team explained that nacreous or polar stratospheric clouds are relatively rare due to the very specific conditions needed for them to appear. 

Rare Nacreous clouds, known as rainbow clouds, form in the skies over Tynemouth Priory  in the north east of England
Image: Rare nacreous clouds, known as rainbow clouds, form in the skies over Tynemouth Priory
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Rare "rainbow clouds" have been spotted in skies above the UK.

A number of people across the country have been treated to views of the colourful nacreous clouds this week.

Lindsay Mackenna took some pictures of the natural phenomenon above Edinburgh on Tuesday night, describing the iridescent clouds as "gorgeous".

She told Sky News: "I'm 65 and I've only seen this once before, but never at sunset.

"I couldn't believe what I was seeing. It's amazing what nature can produce - just wonderous."

Rainbow clouds/nacreous clouds. Pic: Lindsay Mackenna
Image: The colourful clouds pictured in Edinburgh. Pic: Lindsay Mackenna
Rare Nacreous clouds, known as rainbow clouds, form in the skies off the coast of Tynemouth in the north east of England
Image: The rare clouds off the coast of Tynemouth

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The Sky News weather team explained that nacreous or polar stratospheric clouds are relatively rare due to the very specific conditions needed for them to appear.

More on Scotland

They form high up in the stratosphere when temperatures are -78C (-108F), so you are more likely to see them in polar regions during the winter.

Nacreous clouds. Pic: Jo Wheeler
Image: Pic: Jo Wheeler
Nacreous clouds. Pic: Rachel Stewart
Image: Pic: Rachel Stewart

These shimmering "mother of pearl" clouds are some of our highest clouds, forming around 12 to 19 miles (19km to 31km) above the earth.

Nacreous clouds are best seen before sunrise and after sunset when the sun is just below the horizon.

Nacreous clouds. Pic: Whitfield Benson
Image: Pic: Whitfield Benson
Nacreous clouds. Pic: Whitfield Benson
Image: Pic: Whitfield Benson

The pastel-rainbow colours are due to iridescence, when tiny ice crystals or water droplets cause sunlight to be diffracted and spread out, creating colours similar to those seen on soap bubbles or oil.

Cloud iridescence itself is actually a fairly common phenomenon at lower levels in our atmosphere, and can often be seen on the edges of clouds near to the sun or moon, usually in altocumulus, cirrocumulus, lenticular and cirrus clouds.