The green flash occurs when, under certain atmospheric conditions, the top segment of the low sun is visibly green. It is surrounded—in at least a few minds—by an air of mystery. I describe a simple experiment that demonstrates different aspects of the green flash. The experiment uses an odd-shaped, water-filled, fish tank to simulate the refractive properties of the atmosphere; milk powder added to the water mimicks the atmosphere’s scattering properties. A circular white-light source is viewed through the fish tank and the combination of refraction and scattering makes one end of the light source look green. The setup also allows experimentation with mirage effects, thereby drawing attention to their often neglected contribution to the green flash.
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The green flash is normally observed from the coast, as the horizon is then particularly low and the light path through the atmosphere particularly long. But it can also be seen over land, best from places with a low horizon such as airplanes, mountain tops, and tall buildings (see Ref. 4).
Lord Kelvin (W. Thomson), for example, observed a Blue Flash from his hotel room in the Alps as the sun was rising over Mont Blanc (Ref. 50).