Geography
Gurugram: one
dead, three contused once lightning strikes tree
· It may be a
terribly speedy and big discharge of electricity within the atmosphere. its
the method of prevalence of a natural ‘electrical discharge of terribly short
length and high voltage between a cloud and therefore the ground or among a
cloud’, in the middle of a bright flash and sound, and generally thunderstorms.
· Inter cloud or
intra cloud (IC) lightning ar visible and harmless.
· It is cloud to
ground (CG) lightning, that is harmful because the ‘high electrical voltage and
electrical current’ results in electrocution.
Process:
· It may be a
results of the distinction in electrical charge between the highest and bottom
of a cloud.
· The lightning-generating
clouds ar usually concerning 10-12 kilometer tall, with their base concerning
1-2 kilometer from the Earth’s surface. The temperatures at the highest vary
from -35°C to -45°C.
· As vapor moves
upwards within the cloud, it condenses into water because of decreasing
temperatures. a large quantity of warmth is generated within the method,
pushing the water molecules any up.
· As they move
to temperatures below zero, droplets turn out to be little ice crystals. As
they continue upwards, they gather mass, till they become thus significant that
they begin downward-sloping.
· It results in
a system wherever smaller ice crystals move upwards whereas larger ones come
back down. The ensuing collisions trigger unharness of electrons, {in a|during
a|in an exceedingly|in a terribly} method very just like the generation of
electrical sparks. The moving free electrons cause additional collisions and
additional electrons resulting in a series reaction.
· The method
ends up in a scenario within which the highest layer of the cloud gets charged
whereas the center layer is charged.
· In very little
time, a large current, of the order of lakhs to various amperes, starts to flow
between the layers.
· It produces
heat, resulting in the heating of the air column between the 2 layers of cloud.
· It is
attributable to this heat that the air column appearance red throughout
lightning.
The heated air column expands and produces shock
waves that end in thunder sounds.
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