Sun Dog
A sun dog (or sundog)
or mock sun, formally called a parhelion (plural parhelia)
in meteorology, is an atmospheric optical phenomenon that
consists of a bright spot to the left or right of the Sun. Two sun dogs
often flank the Sun within a 22° halo.
The sun dog is a member of the family
of halos, caused by the refraction of sunlight by ice
crystals in the atmosphere. Sun dogs typically appear as a pair of subtly
colored patches of light, around 22° to the left and right of the
Sun, and at the same altitude above the horizon as the Sun. They can be
seen anywhere in the world during any season, but are not always obvious or
bright. Sun dogs are best seen and most conspicuous when the Sun is near the
horizon.
A Sun
halo, a circle of light that creates a circle 22° wide around the Sun, is a
related phenomenon. As with sundogs, hexagonal ice crystals suspended in
cirrostratus clouds refract sunlight to create the halo, sometimes also called
an ice bow, nimbus, or gloriole. Unlike sundogs, which generally only be seen
when the Sun is near the horizon, the halo is visible even when the Sun is
high. Sundogs appear along the 22° halo and disappear as the Sun rise. There
are also moon dogs that appear alongside the moon and are formed by lunar light
passing through ice crystals. Moon dogs, or paraselenae, are not observed as
often as sundogs because they are visible when the moon is bright and
because they appear during the night.
Origin
Sundogs are formed from hexagonal ice
crystals in high and cold cirrus clouds or, during very cold weather, by ice
crystals drifting in the air at low levels. These crystals act as prisms,
bending the light rays passing through them. As the crystals sink through the
air they become vertically aligned, refracting the sunlight horizontally so
that sundogs are observed.
Darun
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