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A
7° high sun flanked by bright parhelia.
Sundogs (parhelia, mock suns) are, with the 22º halo, the most
frequent of the halos. Look for them, especially when the sun is low,
at each side and about 22° away. This is the same distance
or more**
than the common circular halo.
Sundogs reveal that the clouds are hosting horizontal plate crystals.
These plates drift slowly downwards like leaves with their large faces
almost horizontal.
Sundogs are formed when light passes through crystal side faces inclined
at 60° to each other. The rays, like those of the 22°
halo, are deviated by up to 50° but those near to the minimum
deviation condition of near**
to 22° are the most numerous and they form the very bright sundog
inner edges. Sundogs are often brightly coloured because the crystals
refract each colour by a different amount.
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In
the simulation a parhelic circle
and a sun pillar, also produced
by plate crystals, are visible. Some poorly oriented crystals
produced the 22° reference halo. Sundogs often curve upwards
in photographs and simulations, this is a projection effect
and they are always at the same altitude as the sun.
** Unlike
the 22° circular halo, sundogs are not always
22° from the sun. As the sun gets higher
they pull away from the 22° halo because the rays forming them
become increasingly skewed relative to the crystal axis. Take
a look at Tom Eklund's image
when the sun was 43º high. |
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