- UCAR Home
- About Us
- For Staff
Margaret LeMone | 7 January 2010 • Have you ever looked up in the sky and seen something totally surprising? While walking near our office with my friend Sandra on the early afternoon of 29 December 2009, I pointed out a partial halo around the sun. The halo’s radius (the distance between the sun and the halo) was 22 degrees, or about the width of your hand if you held it at arm’s length and spread your fingers fully. On the right side of the halo, there was a sundog or “parhelion” —a bright spot at the same height above the horizon as the sun.
Figure 1. Circumzenithal arc, looking straight up.
The optics show evolved further as we kept watching. About 2:00 p.m., looking toward the other side of the sky, we witnessed a parhelic circle, along with a sundog-like bright patch in the middle of it (Figure 2, below).
This bright spot is called a “120 degree parhelion” because it lies 120 degrees horizontally from the Sun, or about one-third the way around the horizon. In contrast, the “normal” parhelion, or sundog, lies only 22 degrees from the sun horizontally. For example, if the Sun had been south-southwest of us (at about 200 degrees on a compass), the bright spot of this 120-degree parhelion would have been at (200 + 120) = 320 degrees, or roughly northwest of us. The more common 22-degree parhelion would have been at (200 + 22) = 222 degrees, or roughly southwest of us.
Figure 2. Parhelic circle and 120-degree parhelion, looking northwest at 2:00 p.m. MST. The parhelic circle is the subtle arc just above the middle of the picture; the 120-degree parhelion on the circle just to the right of the center of the picture.
For the 22-degree halo and for a typical sundog, the light enters one face of a hexagonal crystal and exits at another face angled at 60 degrees to the first face. (If the faces were exactly parallel, the light ray would bend twice, but end up going in the same direction.) Although this refraction is taking place in ice crystals throughout the cloud, we see only the light coming through those crystals that are located about 22 degrees from the Sun. Near-vertical crystals contribute to the sides of the halo, and near-horizontal crystals contribute to its top and bottom, with crystals at other orientations contributing to the rest of the halo. Similarly, light coming from the vertical crystals forms the sundogs, which are often seen on both sides of the sun.
Because different wavelengths of light are bent at slightly different angles, there is a slight color separation. The light-ray paths for sundogs (parhelia) are similar, with the sides of the ice crystal vertical. Because red light rays are not bent as much as light of shorter wavelengths, the side of a sundog nearer the sun is the redder one.
Wider and wider
What about the parhelic circle, which extends much farther from the Sun than the halos and sundogs discussed above? When light rays reflect off the inside of an ice crystal two or more times, the extra reflections mean that we see the light from crystals located 120 degrees away the Sun.
The parhelic circle is caused by reflection off vertical ice-crystal faces (external reflection). Internal reflections (the light entering the ice crystal and reflecting off a crystal face from the inside) also contribute. For the circumzenithal arc, the light enters the top of a prism whose side faces are perpendicular to the faces at the top and bottom, and exits out a side. Again, the red light bends less than the shorter wavelengths, so the red is closer to the sun.
Wikipedia, the website Atmospheric Optics, and the UCAR-based Windows to the Universe site will give you a great deal more information on these and other optical phenomena. With a little bit of background, you can learn to appreciate the mathematics and physics behind these features as well as their sheer beauty.
Optics 101: Refraction and ice crystals
Below are two mini-tutorials I put together to accompany this post. The first one uses a battlefield analogy to show how a light ray gets bent, or refracted, as it enters a prism. (You don't need to follow the mathematics to understand the analogy!) The second one shows how only a few of the ice crystals in a cloud are oriented in such a way as to produce a halo.
The University Corporation for Atmospheric Research manages the National Center for Atmospheric Research under sponsorship by the National Science Foundation. Any opinions, findings and conclusions, or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.