I will list several phenomena found in Antarctica.
Pastel colours in clouds close to the Sun or Moon reveal the presence of water droplets in the cloud. These shades are called the corona, and the physics is similar to that seen when a drop of oil falls onto the surface of a puddle.
The air temperature in Antarctica is often low enough for water vapour to condense directly out of the atmosphere and form tiny ice crystals which then fall. On a sunny day these catch the sunlight and shine like a sprinkling of diamonds in the sky, hence the name diamond dust. If the crystals are orientated in exactly the right way they can give rise to brilliant halos.
A fogbow is formed in exactly the same way as a rainbow, but the colours overlap in the tiny droplets of water in fog and convert the rainbow back to a colourless bow.
The head of the observer’s shadow, or the more distant shadow of an aeroplane on cloud below is often surrounded by a bright glow called the glory. The shadows of other people do not show this effect.
If the atmosphere is very clear, the final sliver of the setting sun may turn a vivid green or blue colour. This is the green flash, and is caused by the atmosphere acting like a prism and spreading the solar light into a spectrum of colours of which only the green or blue is seen, the others being below the horizon. The Sun sets and rises so slowly at the South Pole that you can see the green flash for hours at a time near the equinoxes.
A halo is a ring or pillar of light around the Sun or the Moon. Halo displays are frequent in Antarctica and are particularly bright when they form in diamond dust. There are many different types of halo, ranging in simple rings with diameters of 22° or 46°, pillars above the sun or moon, sun dogs or parhelia on either side of the Sun or Moon and arcs like rainbows high in the sky.
A moonbow is much rarer than a rainbow, as it requires the moon to be close to full. Antarctic moonbows are very rare indeed.
· 9 years ago