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CLOUD TYPES
There are 3 main types of clouds: cumulus, stratus & cirrus.
They can be categorized according to their shape & altitude above sea level.
Cloud Formation: Warm moist air rises, cools and water vapor condenses on condensation nuclei.
The air then stops rising when its temperature is equal to the atmospheric air.
The cloud will flatten and wind will spread it horizontally.
Altitude
High
altitude
Middle
altitude
Name
Composition
Precipitation
cirrus
wispy, feathery
ice crystals
none
cirrostratus
thin, long, transparent,
creates halo around sun or moon
ice crystals
none
cirrocumulus
thin, white, billowy -rare
predicts snow or rain
ice crystals
none
altocumulus
wavy rows, layered,
gray-white
water
very little
altostratus
gray, sheet-like, thin
layers
water
rain or snow
nimbostratus
large, thick, dark, gray
storm cloud
ice & water
steady &long
rain or snow
cumulonimbus
dark, towering, storm cloud
thunderheads
ice & water
heavy rain,
hail, lightning
stratus clouds that touch
the ground.
water
drizzle
fog
Low
altitude
Description
stratocumulus
rippled, irregular layers,
gray-white
Associated with cold fronts
water
light rain, snow
& drizzle
stratus
low, uniform gray sheets
Cover large areas & block sun
Can form from risen fog
water
drizzle
cumulus
white, puffy, cottony
Fair weather cloud
water
none
CLOUD TYPES
There are 3 main types of clouds:
They can be categorized according to
:
The air then stops rising when its temperature is equal to the atmospheric air.
The cloud will flatten and wind will spread it horizontally.
Altitude
Name
Description
Composition
Precipitation
High
altitude
thin, long, transparent,
thin, white, billowy -rare
Middle
altitude
wavy rows, layered,
gray-white
very little
gray, sheet-like, thin
layers
rain or snow
nimbostratus
dark, towering, storm cloud
heavy rain,
hail, lightning
fog
Low
altitude
rippled, irregular layers,
gray-white
Associated with cold fronts
low, uniform gray sheets
Can form from risen fog
white, puffy, cottony
water
water
light rain, snow
& drizzle