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PRESENTED BY
M. Fasihud Din Nauman
     (Roll. No: 29)
Environmental Science
    (4TH- Semester)
Clouds
   visible mass of liquid droplets or
frozen crystals made of water and/or
       aerosols is called cloud.
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)
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.
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
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
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)
Cloud Types
TYPES OF CLOUDS
♦ High-level clouds:
  ♣ cirrus ♣ cirrostratus ♣ cirrocumulus

♦ Mid-level clouds:
  ♣ altostratus     ♣ altocumulus

♦ Low-level clouds:
   ♣ stratus        ♣ cumulus
HIGH-LEVEL
  CLOUDS
High Clouds (Family A)
 Composed of ice crystals (Cirrostratus)
 Thin and wispy (Cirrus)
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.
CIRRUS
   Thin, featherlike clouds that are made of ice
crystals high in the atmosphere. Usually means a
         change in the weather is coming.
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
CIRROSTRATUS
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.
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
CIRROCUMULUS
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
MID-LEVEL
 CLOUDS
Mid-Level Clouds
 Composed of water droplets and ice
  crystals
ALTOSTRATUS
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.
Altocumulus Clouds
LOW-LEVEL
 CLOUDS
Low-Level Clouds
 Composed mostly of water droplets
STRATUS
Sheets of low, grey clouds that bring light
          snow, rain, or drizzle.
NIMBOSTRATUS
NIMBOSTRATUS
  Thicker layer than stratus clouds that
completely block out the sun. They cause
          steady rain or snow.
CUMULUS
White and puffy clouds that usually
       mean good weather.
CUMULONIMBUS
CUMULONIMBUS
Dark, towering clouds that are also called
 “thunderheads”. These clouds produce
 heavy rain, thunderstorm, and lighting.
Cumulonimbus
PRECIPITATION
Process by which water falls to Earth
from clouds in the atmosphere in the
  form of rain, snow, sleet, or hail.
TYPES OF
PRECIPITATION
As raindrops
 fall from the
clouds they join
   with other
   droplets of
     water.

  This causes
 the raindrops
   to grow in
      size.

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Ppp on clouds and their classification

  • 1. PRESENTED BY M. Fasihud Din Nauman (Roll. No: 29) Environmental Science (4TH- Semester)
  • 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)
  • 9. TYPES OF CLOUDS ♦ High-level clouds: ♣ cirrus ♣ cirrostratus ♣ cirrocumulus ♦ Mid-level clouds: ♣ altostratus ♣ altocumulus ♦ Low-level clouds: ♣ stratus ♣ cumulus
  • 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
  • 21. Mid-Level Clouds  Composed of water droplets and ice crystals
  • 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.
  • 26. Low-Level Clouds  Composed mostly of water droplets
  • 27.
  • 28. STRATUS Sheets of low, grey clouds that bring light snow, rain, or drizzle.
  • 30. NIMBOSTRATUS Thicker layer than stratus clouds that completely block out the sun. They cause steady rain or snow.
  • 31.
  • 32. CUMULUS White and puffy clouds that usually mean good weather.
  • 34. CUMULONIMBUS Dark, towering clouds that are also called “thunderheads”. These clouds produce heavy rain, thunderstorm, and lighting.
  • 36. PRECIPITATION Process by which water falls to Earth from clouds in the atmosphere in the form of rain, snow, sleet, or hail.
  • 38. As raindrops fall from the clouds they join with other droplets of water. This causes the raindrops to grow in size.