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Clouds
are formed when moist air is carried aloft by warm air currents rising
from the earth's surface during the day.
When this air reaches high altitudes where the temperature and barometric
pressure are lower than at the earth's surface,
the moisture comes out of the rising air and forms the water droplets
we see as clouds. These clouds are very short-lived,
though, and they usually disappear within minutes after they are formed
as their water droplets mix with drier air and
evaporate. Thus, during the daytime, clouds are continually being formed
and then evaporated.
At night, when the surface of the earth cools, the cloud-producing process
cuts off. The existing clouds continue to
evaporate, but they are not replaced by new ones. The result: cloudless
skies in the morning.
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