Lightning
When Liquid water droplets within a cloud freeze into ice,
electrical charges develop. Ice crystals become positively
charged, while the remaining liquid droplets take on a
negative charge. Soon the whole cloud becomes charged:
positive charges collect in the icy cloud top;negative
charges accumulate in the lower, warmer parts of the
cloud. Normally the ground is also negatively charged, but
the concentration of electrons in the lower cloud repels
the negative ground charge(like charges repel; opposites
attract), leaving positvely charged ground directly
beneath the cloud. The gathering electrical charges build
voltages as high as 100 million volts within the cloud and
between cloud and ground. Air can seperate voltages as
great as 3,000 volts per foot,or 15 million volts per mile,
but when voltage exceed these values, lightning results.
Sequence
Lightning begins as a relatively weak and faintly visible
leader stroke makes its way down from a cloud base to
(1/100 second later) a tree, the ground, or several targets,
completing an electrical pathway between cloud and
ground. A massive return stroke shoots up along the
leader path at one-sixth the speed of light. Return strokes
from several ground targets may join several hundred feet
up, forming branched lightning. The concentration of
electricity in a path 1"(2.5cm) across heats the air almost
instantaneously to tens of thousands of degrees(hotter
and brighter than the surface of the Sun). We See the
glowing channel as a cloud-to-ground lightning flash,while
the sudden heating and expansion of the air makes
thunder. Other varities, such as in-cloud lightning and
cloud-to-cloud lightning, discharge in a similar manner.
Many more cloud lightning discharges occur than flashes
to the ground; most often-especially at night-lightning
is seen as illumination inside a storm.
Significance
Distant lightning indicates instability sufficient for a
thunderstorm to develop. Lightning that is close enough
for thunder to be heard indicates that a storm may be
imminent. Sound travels at 5 seconds per mile (3 seconds
per Km). When a lightning flash is seen and its thunder
follows 15 seconds later; the lightning is 3 miles(5 Km)
away.
Season and Range
Lightning occurs year-round in warm climates, and mainly
in summer where winters are cold.