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By Zach Kraus



 http://www.layoutsparks.com/1/142820/rain-
 cloud-falling-drops.html
Adiabatic Temperature Changes and
       Expansion and Cooling
• Air cools when it expands and it warms when
  it compresses
• Dry adiabatic rate is 10ᵒ per every 1000
  meters
• Wet adiabatic rate is 5ᵒ-8ᵒ per every 100
  meters

modelliabridal.net
Orographic Lifting
• When elevated land, like mountains, blocks
  the airflow
• which can cause adiabatic cooling which
  makes clouds and precipitation



• ag.arizona.edu
Frontal Wedging
• When cool dense air makes less dense warmer
  air rise above the cooler air




• geo.hunter.cuny.edu
Convergence
• Airflow from more than one direction, usually
  up
• Leads to adiabatic cooling and the formation
  of clouds



• ww2010.atmos.uiuc.edu
Localized Convective Lifting
• When warm pockets of air around cooler air
  pushes the warm air up




• rst.gsfc.nasa.gov
Stability
                                 splendidlittlestars.blogspot.com


• Stable air resists vertical movement while
  unstable air rises freely
• The most stable air is when air temperature
  rises with height which is called a temperature
  inversion
• Thin clouds are formed when stable air is
  forced into the atmosphere, compared to
  puffy clouds formed from unstable air
Condensation
• Can be in the forms of dew, fog, or clouds
• Air must be saturated for any kind of
  condensation
• Must have a surface to condensate on




                   usefilm.com
Types of Clouds
•   Classified on the basis of their form and height
•   Cirrus clouds are white, thin, and high
•   Cumulus clouds are round individual clouds
•   Stratus clouds are sheets that cover up a lot of
    the sky



               electricscotland.com
High Clouds
• First type, Cirrus clouds are very thin and
  wispy
• Second type, Cirrocumulus that have fluffy
  masses
• Last type, Cirrostratus clouds are flat layers




                                         eo.ucar.edu
Middle Clouds
• Range from about 2,000-6,000 meters
• Altocumulus clouds are thicker and denser
  than cirrocumulus
• Altostratus clouds creates a white blanket that
  covers the sky




           eo.ucar.edu
eo.ucar.edu


     Low Clouds
• Stratus, stratocumulus, and nimbostratus are
  the three types of low clouds
• Stratus clouds are like foggy layers of clouds
• Stratocumulus clouds appear as long patches
  of clouds
• Nimbostratus clouds are usually the clouds
  that create precipitation and are made of
  stable air
Clouds of Vertical Development
• Associated with unstable air
• Usually cumulus clouds that grow upward and
  turns into cumulonimbus cloud that usually
  makes rain and thunderstorms



   prwatch.org
Fog
• No difference between fog and clouds, fog is
  defined as a cloud with its base close to the
  ground
• Sometimes made by warm moist air moves
  over cold ground
• May occur when cool air moves over warm
  water

            stuffintheair.com
Cold Cloud Precipitation
• The Bergeron procedure relies on super
  cooling and supersaturating to chill the water
  in the air
• Super cooled water is water under 0 and will
  readily freeze if touches a solid object




                       stockphotopro.com
Warm Cloud Precipitation
• The collision-coalescence process forms
  raindrops in warm clouds




         frrl.wordpress.com
Rain and Snow
• The term rain means drops of water that fall
  from clouds and need to be .5 mm, rain
  smaller than that is considered drizzle
• When the temperature is lower 6 sided ice
  crystals that are fluffy and white fall from
  clouds

           its.caltech.edu
Sleet, Glaze, and Hail
• Sleet is falling pieces of ice that are small and
  almost see through
• Glaze is raindrops that freeze when they hit
  the ground
• Hail is pieces of ice that grow bigger and
  bigger as they fall through the air


                  askpari.wordpress.com
school.discoveryeducation.com

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Clouds and precipitation

  • 1. By Zach Kraus http://www.layoutsparks.com/1/142820/rain- cloud-falling-drops.html
  • 2. Adiabatic Temperature Changes and Expansion and Cooling • Air cools when it expands and it warms when it compresses • Dry adiabatic rate is 10ᵒ per every 1000 meters • Wet adiabatic rate is 5ᵒ-8ᵒ per every 100 meters modelliabridal.net
  • 3. Orographic Lifting • When elevated land, like mountains, blocks the airflow • which can cause adiabatic cooling which makes clouds and precipitation • ag.arizona.edu
  • 4. Frontal Wedging • When cool dense air makes less dense warmer air rise above the cooler air • geo.hunter.cuny.edu
  • 5. Convergence • Airflow from more than one direction, usually up • Leads to adiabatic cooling and the formation of clouds • ww2010.atmos.uiuc.edu
  • 6. Localized Convective Lifting • When warm pockets of air around cooler air pushes the warm air up • rst.gsfc.nasa.gov
  • 7. Stability splendidlittlestars.blogspot.com • Stable air resists vertical movement while unstable air rises freely • The most stable air is when air temperature rises with height which is called a temperature inversion • Thin clouds are formed when stable air is forced into the atmosphere, compared to puffy clouds formed from unstable air
  • 8. Condensation • Can be in the forms of dew, fog, or clouds • Air must be saturated for any kind of condensation • Must have a surface to condensate on usefilm.com
  • 9. Types of Clouds • Classified on the basis of their form and height • Cirrus clouds are white, thin, and high • Cumulus clouds are round individual clouds • Stratus clouds are sheets that cover up a lot of the sky electricscotland.com
  • 10. High Clouds • First type, Cirrus clouds are very thin and wispy • Second type, Cirrocumulus that have fluffy masses • Last type, Cirrostratus clouds are flat layers eo.ucar.edu
  • 11. Middle Clouds • Range from about 2,000-6,000 meters • Altocumulus clouds are thicker and denser than cirrocumulus • Altostratus clouds creates a white blanket that covers the sky eo.ucar.edu
  • 12. eo.ucar.edu Low Clouds • Stratus, stratocumulus, and nimbostratus are the three types of low clouds • Stratus clouds are like foggy layers of clouds • Stratocumulus clouds appear as long patches of clouds • Nimbostratus clouds are usually the clouds that create precipitation and are made of stable air
  • 13. Clouds of Vertical Development • Associated with unstable air • Usually cumulus clouds that grow upward and turns into cumulonimbus cloud that usually makes rain and thunderstorms prwatch.org
  • 14. Fog • No difference between fog and clouds, fog is defined as a cloud with its base close to the ground • Sometimes made by warm moist air moves over cold ground • May occur when cool air moves over warm water stuffintheair.com
  • 15. Cold Cloud Precipitation • The Bergeron procedure relies on super cooling and supersaturating to chill the water in the air • Super cooled water is water under 0 and will readily freeze if touches a solid object stockphotopro.com
  • 16. Warm Cloud Precipitation • The collision-coalescence process forms raindrops in warm clouds frrl.wordpress.com
  • 17. Rain and Snow • The term rain means drops of water that fall from clouds and need to be .5 mm, rain smaller than that is considered drizzle • When the temperature is lower 6 sided ice crystals that are fluffy and white fall from clouds its.caltech.edu
  • 18. Sleet, Glaze, and Hail • Sleet is falling pieces of ice that are small and almost see through • Glaze is raindrops that freeze when they hit the ground • Hail is pieces of ice that grow bigger and bigger as they fall through the air askpari.wordpress.com