Iridescence

2010.08.20

Sitting in the garden in Monetier.  Julie, Pierre-Yves, Manon and me are having some coffee in the garden. Hardly visible layers of milky white cirrus start to appear in the sky…  Half an hour later strange forms deploy and disappear… In combination with the sun they start to color in millions of tints…  It was a strong coffee…

When parts of clouds are thin and have similar size droplets, diffraction can make them shine with colours like a corona. In fact, the colours are essentially corona fragments. The effect is called cloud iridescence or irisation, terms derived from Iris the Greek personification of the rainbow. The usually delicate colours can be in almost random patches or bands at cloud edges. They are only organised into coronal rings when the droplet size is uniform right across the cloud. The bands and colours change or come and go as the cloud evolves. They occur most often in altocumulus, cirrocumulus and especially in lenticular clouds. Iridescence is seen mostly when part of a cloud is forming because then all the droplets have a similar history and consequently have a similar size. Sometimes iridescence can be seen far from the sun but is most frequent near to it. As for coronas, search safely by hiding the sun behind a building and, even better, also viewing the reflection of the sky in water.

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Crystallized photons

2009.10.20

When sunlight meets oriented plate crystals, the same crystals that form sundogs a circumzenithal arc is formed. The refraction of rays nearly parallel rays through faces inclined at 90° produces very pure and well separated prismatic colours. The colours of the circumzenithal arc are purer than those of the rainbow.

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Last week optics…

2009.03.19

Distrail:

We’ve all observed the worrying proliferation of condensation trails, or ‘contrails’, criss-crossing our skies in the wake of high-altitude aircraft. They look like man-made scars across the blue. But how many have noticed the much less common but related cloud effect, known as a ‘distrail’?

Short for ‘dissipation trail’, this is not so much a cloud, as a gap in cloud cover. It can appear when an aircraft happens to pass through a fairly thin cloud layer composed of ’supercooled’ droplets. These are in unfrozen, liquid form, even though temperatures are well below 0degC. Water droplets can stubbornly refuse to freeze when there is a lack of air-borne particles to act as nuclei onto which the ice crystals can start forming.

As an aircraft climbs or descends through one of these supercooled clouds, the turbulence of its wake and the many minute particles contained in its exhaust encourage the cloud’s droplets to freeze. This happens when some of the particles act as the nuclei onto which the droplets can start freezing. As the crystals form, they grow in size and fall below. Left behind, is a just gap in the cloud – the distrail.

Or in meteorological terms: dissipation trail—(Or distrail.) A clearly delineated limpid lane forming behind an aircraft flying in a thin cloud layer; the opposite of a condensation trail.

The heat of combustion of the aircraft fuel, released into the swept path by the exhaust stacks of the aircraft, can, under certain conditions, evaporate existing clouds (if not too dense) and yield a distrail. Clouds of low liquid water content and relatively high temperature are susceptible to distrail formation but the phenomenon is comparatively rare.

Pictures taken on March 5th (optics with circumscribed halo, the first 9 pictures), on March 7th (distrails…, pictures 10 to 15) and March 18th (picture 16 to 45…morning Sundogs, Shanti… our own dog, a twisted contrail part, some faint iridescence, early frozen grass, a small part of the world through a drop of water and some afternoon sundogs with a would be blue like parhelic attachment…)

Unfortunately I had to “work” this afternoon which probably led to missing an opportunity in photographing some nice displays in the sky.

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