Clouds
Large amount of water evaporates each day from the
surface of the sea. This is the principal source of atmospheric moisture. Cool
moisture laden air, gets collected around particles like dust, salt content
from the sea, smoke etc., and forms clouds. Sometimes, mixing of warmer and
cooler air also produces clouds. A visible mass of condensed water vapour
floating in the air above the ground level is called a cloud. The three layers
of atmosphere such as troposphere, stratosphere and mesosphere are specific
locations of clouds.
According to their height, clouds are classified into
the following types
·
High clouds (6-20km Height)
·
Middle clouds (2.5km-6km Height)
·
Low clouds (ground surface to 25 km height)
These major types of clouds are further divided
into different types on the basis of shape and structure.
Cirrus:Detachedcloudsintheformof white delicate fibrous silky filaments
formed at the high sky (8000 meters to 12000 meters) are called Cirrus clouds.
These clouds are dry and do not give rainfall.
Cirro-cumulus:
White
patched, sheet or layer like clouds
composed of ice crystals.
Cirro-stratus:
Smooth
milky transparent whitish clouds
composed of tiny ice crystals.
Alto
-stratus: Thin sheets of grey or blue
coloured clouds in uniform appearance. consisting of frozen water droplets
Alto-cumulus:
clouds
fitted closely together in parallel
bands, called as 'Sheep clouds' or wool pack clouds.
Nimbo
stratus: These are clouds of dark colour
very close to the ground surface associated with rain, snow or sleet.
Strato-cumulus:-Greyorwhitishlayer of non-fibrous low clouds found in
rounded patches at an height of 2500 to 3000 metres, associated with fair or
clear weather
Stratus:-
Dense,
low lying fog-like clouds associated
with rain or snow
Cumulus:-
Dome-shaped
with a flat base often resembling a
cauliflower, associated with fair weather
Cumulo-
nimbus:- Fluffy thick towering
thunderstorm cloud capable of producing heavy rain, snow, hailstorm or
tornadoes
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