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    • “mock suns” or “parhelia

      • A sundog is similar to a rainbow and more common than rainbows. Sometimes, they look like bright rainbows or colorful spots on either side of the Sun. Other times, they are brighter and actually look like two extra Suns. Sundogs are also known as “mock suns” or “parhelia,” which means “with the Sun.”
      www.almanac.com/what-are-sundogs-rainbows-beside-sun
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  2. Jul 25, 2006 · A sundog is a concentrated patch of sunlight occasionally seen about 22° to the left or right of the Sun. Sundogs often form in pairs on either side of our daytime star when sunlight refracts through icy clouds containing hexagonal platecrystals aligned with their large, flat faces parallel to the ground.

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  3. Oct 1, 2024 · Sundogs are also known as “mock suns” or “parhelia,” which means “with the Sun.”. The most common name, however, for these bright lights that faithfully follow the Sun is “sundogs.”.

    • What are some common names for sundogs?1
    • What are some common names for sundogs?2
    • What are some common names for sundogs?3
    • What are some common names for sundogs?4
    • What are some common names for sundogs?5
  4. en.wikipedia.org › wiki › Sun_dogSun dog - Wikipedia

    A sun dog (or sundog) or mock sun, also called a parhelion [1] (plural parhelia) in atmospheric science, is an atmospheric optical phenomenon that consists of a bright spot to one or both sides of the Sun. Two sun dogs often flank the Sun within a 22° halo.

    • Moon Dog
    • Common Names For A Sun Dog
    • Ice Crystals That Refract Sunlight
    • Significance of A Sun Dog
    • Formation of A Sun Dog

    The sun dog, as it’s more commonly called, is a form of atmospheric optical phenomena. The formation occurs due to light scattering from air particles or larger entities, including ice crystals. These crystals, which are hexagonal in shape, can refract light in a horizontal direction with respect to the Sun, producing an optical effect known as a s...

    A sun dog is an optical phenomenon that appears as a bright patch of light on the sky near the sun. It is in fact part of the same family as halos. It appears in the sky when the sun is very low in the sky, often as a ring of light either side of the sun. Common names for sundogs include sunbow, mock sun, and phantom sun. It is a fascinating phenom...

    Ice crystals that refract sunlight can create a fascinating effect. They can appear anywhere in the sky, but are most visible when the Sun is low on the horizon. Typically, they appear red towards the sun and green or blue beyond. The effect is similar to that of a sun halo, a circle of light that surrounds the Sun. This is caused by hexagonal ice ...

    Sun dogs are a type of halos, which are formed by the refraction of sunlight by ice crystals in the atmosphere. They typically appear as two small, subtly colored patches of light on either side of the Sun at the same altitude above the horizon as the Sun. You can observe them anywhere in the world. However, they are most prominent when the Sun is ...

    Sun dogs form when sunlight is refracted through an ice crystal in the atmosphere. Most ice crystals are hexagonal or plate shaped. The hexagonal shape makes it easier for light to be refracted through the crystal, which gives rise to a sun dog. The hexagonal shape also allows the ice crystals to wobble back and forth, much like a maple leaf. This ...

  5. Oct 29, 2023 · In this guide, we‘ll explore what creates sundogs, how to spot them, their role in weather forecasting, and ways to capture their fleeting beauty. We‘ll also unravel some of their mythic history and dive into the optical science powering their radiance. After reading this, you‘ll be an expert sundog spotter too.

  6. Sun dogs are known as parhelia (singular: parhelion) in the scientific community, which comes from the Greek words meaning "beside the Sun." Other common names for sun dogs include mock or phantom suns.

  7. Sep 24, 2024 · A: Sundogs, also known as mock suns or parhelia, are an atmospheric optical phenomenon featuring bright spots on either side of the Sun within a 22° halo. They occur when sunlight refracts off hexagonal ice crystals in the atmosphere, typically found in cirrus or cirrostratus clouds, or as diamond dust in cold weather.

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