Ice Halo Tracker

Ice halos

Rings, arcs and bright spots in the sky, made by sunlight passing through tiny ice crystals.

What they are

High, thin cloud such as cirrostratus is made of ice crystals a fraction of a millimetre across. Most of them are small hexagonal prisms: flat plates or long columns. Light that enters one face of a crystal and leaves through another is bent by a fixed amount, and millions of crystals together send that light to fixed places in the sky. That is a halo.

Low ice fog near the ground, called diamond dust, makes the brightest and most varied displays, because its crystals are often large and very regular.

Which way the light goes

The two ends of a hexagonal crystal are its basal faces, numbered 1 and 2; the six sides are numbered 3 to 8. A ray path lists the faces a ray passes through:

How the crystals fall

Which halos appear depends on how the crystals are oriented as they drift down:

The height of the sun matters too: the circumzenithal arc needs the sun below 32°, the circumhorizontal arc needs it above 58°, and the sun dogs move further out from the 22° halo as the sun climbs.

The halos on the list

Loading…

More to read and see