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Reflection halo twins: subsun and supersun.

Gunther P Können1, Siebren Y van der Werf

  • 1konnen@planet.nl

Applied Optics
|October 22, 2011
PubMed
Summary

A rare atmospheric optical phenomenon, the supersun, appears as a vertical band above the setting sun. It is caused by light reflecting off ice crystals when the sun is below the horizon, visible from high altitudes.

Area of Science:

  • Atmospheric optics
  • Meteorology
  • Optical phenomena

Background:

  • A vertical halo-like structure, termed the supersun, is observed from aircraft above the setting sun.
  • The supersun is the optical counterpart to the well-known subsun phenomenon.
  • Unlike the subsun (reflections from ice crystals illuminated from above), the supersun arises from crystals illuminated from below.

Purpose of the Study:

  • To explain the formation and geometrical properties of the supersun.
  • To investigate the conditions under which the supersun is visible.
  • To simulate the supersun's appearance and radiance distribution.

Main Methods:

  • Analysis of the geometrical optics governing light reflection from oriented ice crystals.
  • Utilizing an extended atmospheric ray-tracing program for simulations.

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  • Considering the effect of Earth's curvature on the reflecting crystal ensemble.
  • Main Results:

    • The supersun forms when the sun is below the true horizon and viewed from elevated positions.
    • Earth's curvature causes ice crystals to act as a hollow mirror, creating the supersun.
    • The supersun appears as a uniform vertical band extending upwards from the sun.

    Conclusions:

    • The supersun is a distinct atmospheric halo resulting from specific ice crystal orientations and illumination.
    • Its visibility is contingent on observer altitude and the sun's position relative to the horizon.
    • Ray-tracing simulations accurately model the supersun's geometric and radiance characteristics.