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Whiteout is a weather condition in which visibility and contrast are reduced by snow and diffuse lighting from overcast clouds.

There are two different forms of a whiteout:

  1. In blizzard conditions, the windblown snow in the air may simply make it too difficult to see very far.
  2. In clear air conditions, when there is no snow falling, diffuse lighting from overcast cloud may cause all surface definition to disappear. It becomes impossible to tell how far away the snowy surface is. In polar regions (and in eg the Scottish Hills in winter) this optical illusion can make whole snow-covered mountains invisible against the background white cloud, and the horizon cannot be identified, slopes cannot be judged for steepness, and snow surfaces cannot be seen. (This effect is accentuated by a smooth surface of fresh-fallen snow). It is only when a dark or coloured object is placed on a snowy surface that the surface can be seen at all. (In less extreme cases, it may suffice to break the snow surface by gently throwing a snowball ahead).

See also


Weather

Whiteout

 

This article is licensed under the GNU Free Documentation License. It uses material from the "Whiteout (weather)".

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