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  2. Crepuscular rays - Wikipedia

    en.wikipedia.org/wiki/Crepuscular_rays

    Crepuscular rays usually appear orange because the path through the atmosphere at dawn and dusk passes through up to 40 times as much air as rays from a high Sun at noon. Particles in the air scatter short-wavelength light (blue and green) through Rayleigh scattering much more strongly than longer-wavelength yellow and red light.

  3. Atmospheric optics - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_optics

    Other colors occur naturally in clouds. Bluish-grey is the result of light scattering within the cloud. In the visible spectrum, blue and green are at the short end of light's visible wavelengths, while red and yellow are at the long end. [20] The short rays are more easily scattered by water droplets, and the long rays are more likely to be ...

  4. File:Sun rays diagram.svg - Wikipedia

    en.wikipedia.org/wiki/File:Sun_rays_diagram.svg

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  5. Sunbeam - Wikipedia

    en.wikipedia.org/wiki/Sunbeam

    Crepuscular rays are noticeable when the contrast between light and dark is most obvious. Crepuscular comes from the Latin word "crepusculum", meaning twilight. [4] Crepuscular rays usually appear orange because the path through the atmosphere at sunrise and sunset passes through up to 40 times as much air as rays from a high midday sun.

  6. File:Sun Rays Through The Clouds.jpg - Wikipedia

    en.wikipedia.org/wiki/File:Sun_Rays_Through_The...

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  7. File:Oblique rays.svg - Wikipedia

    en.wikipedia.org/wiki/File:Oblique_rays.svg

    In short, the angle of incidence affects the heating of the surface in 3 different ways: length of atmospheric track, variable flux and variable reflection For simplicity, the diagram ignores the axial tilt of the Earth, which causes each pole to slip into darkness for around 6 months of the year, and means the equator's ground is generally not ...

  8. File:Weather-few-clouds.svg - Wikipedia

    en.wikipedia.org/wiki/File:Weather-few-clouds.svg

    Original file (SVG file, nominally 48 × 48 pixels, file size: 39 KB) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  9. Circumzenithal arc - Wikipedia

    en.wikipedia.org/wiki/Circumzenithal_arc

    The circumzenithal arc, also called the circumzenith arc (CZA), the upside-down rainbow, and the Bravais arc, [1] is an optical phenomenon similar in appearance to a rainbow, but belonging to the family of halos arising from refraction of sunlight through ice crystals, generally in cirrus or cirrostratus clouds, rather than from raindrops.

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