The sum of all visible wavelengths of light (400-700 nm) so that all colors are blended to appear white to the eye. No pronounced contribution from any one spectral line (or light-emitting element) is
implied.
A major flare in which small parts become visible in white light. This rare continuum emission is caused by energetic particle beams bombarding the lower solar atmosphere. Such flares are usually stro
ng x-ray, radio, and particle emitters.
A condition in which daylight is diffused by multiple reflections between a snow surface and an overcast sky; contrasts vanish, and the observer is unable to distinguish the horizon or any snow surfac
e feature.
An atmospheric optical phenomenon in which the observer appears to be engulfed in a uniformly white glow. (Also called milky weather.) Neither shadows, horizon, nor clouds are discernible; sense of de
pth and orientation is lost; only very dark, nearby objects can be seen. Whiteout occurs over an unbroken snow cover and beneath a uniformly overcast sky, when, with the aid of the snow blink effect, the light from the sky is about equal to that from the snow surface. Blowing snow may be an additional cause. This phenomenon is experienced in the air as well as on the ground.
A condition in which daylight is diffused by multiple reflection between a snow surface and an overcast sky. Contrasts vanish and the observer is unable to distinguish the horizon or any snow surface
feature.