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Clear sky blinks.

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    Clear sky blinks, brightness variations caused by light scattering, are visually detectable and photographable. Atmospheric aerosols significantly enhance these phenomena, aiding surface identification.

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    Area of Science:

    • Atmospheric optics
    • Remote sensing

    Background:

    • Ice blinks and water skies are known phenomena caused by light variations under overcast skies.
    • These variations help observers distinguish between surfaces like ice and water.

    Purpose of the Study:

    • To investigate the occurrence and detectability of clear sky blinks.
    • To model clear sky blinks theoretically.
    • To determine the effect of atmospheric aerosols on clear sky blinks.

    Main Methods:

    • Visual observation and photography of clear sky phenomena.
    • Monte Carlo simulations for theoretical modeling.
    • Analysis of atmospheric aerosol influence.

    Main Results:

    • Clear sky blinks were demonstrated to occur and be visually discernible.
    • Successful photography of clear sky blinks was achieved.
    • Monte Carlo simulations confirmed the theoretical basis for clear sky blinks.
    • A significant enhancement of clear sky blinks was observed in the presence of atmospheric aerosols.

    Conclusions:

    • Clear sky blinks are a real and photographable atmospheric optical phenomenon.
    • Atmospheric aerosols play a crucial role in enhancing clear sky blinks.
    • This phenomenon has potential applications in remote surface identification.