Satellite observations display existing cloud conditions.
The visible picture gives a "camera shot"
from space during the day. The infrared measures temperatures
of the cloud tops (useful during the day or night).
Water vapor shows the percentage of water vapor existing
through the atmosphere.
Satellites take pictures of clouds that move across
the earth, usually from 22,500 miles in space. There
are two types of satellite imagery, visible and infrared.
Visible imagery is used when the satellite takes pictures
of the clouds during the day just like a regular camera.
At night visible imagery is not possible since the
sun is not providing a light source for the picture.
Infrared radiation emitted by clouds is sensed by
the satellite and then converted to temperatures using
mathematical equations. The temperatures are related
to the height of the clouds. Colder temperatures imply
higher cloud tops. Higher cloud tops may be representative
of thunderstorms or fair weather cirrus clouds.