2. Clouds
visible mass of liquid droplets or
frozen crystals made of water and/or
aerosols is called cloud.
3. Cloud Location
Majority of clouds form in the TROPOSPHERE
Clouds can be observed in STRATOSPHERE
and MESOSPHERE
Three layers of atmosphere collectively called
HOMOSPHERE where clouds are present
Clouds are absent in the HETROSPHERE
(Thermosphere and Exosphere)
4. CLOUD FORMATION
Warm air is forced upward, expands then
cools.
As air cools the amount of water vapor needed
for saturation decreases (RH then increases).
RH of 100%, air is saturated
Water vapor begins to condense in tiny drops
around nuclei of dust, salt, and other particles.
Drops of water are so small they are
suspended in air.
Millions of these droplets collect forming
clouds.
5. CLOUDS CLASSIFICATION
There are following components which
summarize the classification system.
♣ Cirro : curl of hair, high
♣ Alto : mid
♣ Strato : layer
♣ Nimbo : rain, precipitation
♣ Cumulo: heap
6. CLOUD CLASSIFICATION
•Clouds are classified by texture and
height from the ground.
SHAPE
Cumulus : cotton ball shaped
Stratus : forms a blanket over
large areas.
Cirrus : feathery or wispy
7. 4 Major families of Clouds
A. High Clouds : above 5-13 km.
B. Middle Clouds : 2-7 km.
C. Low Clouds : 0-2 km.
D. Clouds with vertical development (0-13 km)
11. High Clouds (Family A)
Composed of ice crystals (Cirrostratus)
Thin and wispy (Cirrus)
12. High Clouds Cont…
High-level clouds form above 6 km
The temperatures are so cold at such high
elevations, these clouds are primarily
composed of ice crystals.
High-level clouds are typically thin and
white in appearance, but can appear in a
magnificent array of colors when the sun
is low on the horizon.
13. CIRRUS
Thin, featherlike clouds that are made of ice
crystals high in the atmosphere. Usually means a
change in the weather is coming.
14. High Clouds Cont…
Cirrus (Thin and wispy)
The most common form of high-level clouds are
thin and often wispy cirrus clouds.
Typically found at heights greater than 20,000
feet (6,000 meters)
cirrus clouds are composed of ice crystals that
originate from the freezing of supercooled
water droplets.
Cirrus generally occur in fair weather and point
in the direction of air movement at their
16. CIRROSTRATUS
Cirrostratus clouds form more of a
widespread, veil-like layer. When moon or
sun light passes through the ice crystals of
cirrostratus clouds, the light may dispersed.
17. High Clouds Cont…
Cirrostratus (nearly transparent)
Sheet-like, clouds composed of ice crystals.
Though cirrostratus can cover the entire sky and be up
to several thousand feet thick
They are relatively transparent, as the sun or the
moon can easily be seen through them.
These high-level clouds typically form when a broad
layer of air is lifted by large-scale Convergence
Its presence indicates a large amount of moisture in
the upper atmosphere
These are not precipitation clouds, but signal the
approach of warm front
19. High Clouds Cont…
Cirrocumulus (Cloudlets) (Cc)
Typically found at heights 5 to 12 km.
These clouds signify convection
It includes .
Cirrocumulus usually only forms in patches
23. ALTOSTRATUS CLOUDS
Altostratus clouds “strato” type clouds
having flat and uniform type texture.
Altostratus clouds themselves do not
produce precipitation at the surface.
They frequently indicate warm wave front.