© Alan Dyer
Arenas Valley, New Mexico, United States of America
Latitude: 32° 47' 27'' N
Longitude: 108° 12' 20'' W
01 December 2014 1956 (Local Time)
Camera direction: towards SSE
Image P/S code: P.13.1.4.3
Image I.D.: 6050
This picture shows a circumscribed halo around the moon.
A circumscribed halo is formed when the upper and lower tangent arcs link to form another halo outside of the 22° halo. This occurs only when the elevation of the sun or moon (in this case, the moon) is 32° or more above the horizon. The roughly oval halo touches the 22° halo at its highest and lowest points.
When the light source (the sun or moon) is at an elevation greater than about 50°, the circumscribed halo gradually becomes circular, and at even higher elevations it merges with the 22° halo so that it may be difficult to tell them apart.
When this picture was taken the elevation of the moon was 62° above the horizon and so the circumscribed halo forms a slight oval just outside of the circular 22° halo.
The haloes here have formed due to the refraction of moonlight by ice crystals making up a thin layer of Cirrostratus cloud. Although stars are clearly visible, the complete circle of the 22° halo is evidence that there is a barely visible veil of Cirrostratus nebulosus in the sky.
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This extreme wide-angle photograph from Antarctica shows a 22° halo with two parhelia, or sun dogs, at 2 and 3 on either side. Circling the horizon and lying horizontally through the parhelia and the Sun is the parhelic circle at 4 and 5. At the top and bottom of the 22° halo are an upper tangent arc and a lower tangent arc, which extend around the 22° halo as a faint luminous curve to meet each other and form a circumscribed halo.
Links in the image description will highlight features on the image. Mouse over the features for more detail.