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By: Erinne Finlayson

CLOUDS AND PRECIPITATION
PROJECT
Adiabatic Temperature Change
and Expansion and Cooling
 When air expands it cools but when air is
  compressed it warms.
 The dry adiabatic rate is when cooling and
  heating only affect unsaturated air.
 Farther off the earths surface the less
  pressure.
   http://www.kidsgeo.com/geography-for-kids/0070-adiabatic-temperature-changes.php
Orographic Lifting

 Mountains act like walls to air flow causing
  Orographic lifting.
 Windward side of mountain will be rainy.
 Leeward side will be dryer.
   http://www.examiner.com/outdoorsman-in-salt-lake-city/understanding-why-utah-has-the-
    greatest-snow-on-earth-part-1-orographic-lifting
Frontal Wedging

 Cool and warm air collide producing fronts.
 Cooler air is more dense than warm air.
 Cool air asks like a wall against warmer air.
   http://www.harding.edu/lmurray/113_files/HTML/d2_Earth%20Revised/sld0
    46.htm
Convergence

 The different air masses force air to rise.
 Convergence is when the lower atmosphere
  mix together.
 Florida peninsula is a good example.
 http://keithrogershome.com/Chap8Clds.html
Localized Convective Lifting

 Warmed air
 Warm parcles of air rise and form
  condensation clouds.
 May cause rain showers.

   http://rst.gsfc.nasa.gov/Sect14/Sect14_1c.html
Stability

   Unstable air moves up
   Stable air dose not
   Unstable air= Thunderstorms maybe even
    tornados


http://www.richho
ffmanclass.com/ch
apter4.html
Condensation

 Water vapor changes to liquid. (Gas to liquid)
 Air must be saturated
 Results in dew, fog, or clouds.
 http://www.scottslumber.com/services/window-
  condensation-are-my-windows-defective/
Types of Clouds

 Clouds are formed by form and height.
 Types
   Cirrus (curl of hair) is seen as a white cloud.
   Cumulus (a pile) is seen as rounded separate cloud
    masses. Cauliflower structure.
   Stratus (a layer) seen as sheets or layers that cover
    most or all of the sky.

  http://ed101.bu.edu/StudentDoc/c
  urrent/ED101fa10/jenmks/
High Clouds

 Found over 6,000 meters off of earths surface.
 Cirrus and Cirrostratus are two possible clouds found as a
  high cloud.
 Warning of stormy weather coming.
   http://www.zastavki.com/eng/Nature/Clouds/wallpaper-14253.htm
Middle Clouds

 Found around 2,000-6,000 meters off of
  earths surface.
 These clouds are white or gray.
 They warn of a little snow or drizzle.
   http://acrosstheuniverse.forummotion.com/t862-i-ve-looked-at-clouds-from-both-sides-now
Low Clouds

 Seen as rainy clouds
 Located below 2,000 meters from the Earth’s surface.
 Created when air is forced up.
 Stratus and Stratocumulus are some clouds that can be
    found here.
   http://bmvgallery.com/tag/clouds/
Clouds and Vertical Development

 Made up of unstable air
 These clouds cause showers and thunderstorm.
 A upward movement is strong enough to give many
  clouds a great vertical rang form.
 http://www.uwgb.edu/dutchs/EarthSC102Notes/102Clou
  ds.htm
Fog

 Fog and clouds are the same thing, they are just created
  in different place.
 Fog is the cooling or movement over something cold.
 Fog is found very close to the ground.
 http://helicopterblog.com/?p=276
Cold Cloud Precipitation

 It the ground is 0 degrees Celsius it must be at least -40
  degrees Celsius in the clouds to create snow, hail, ext.
 When ice crystals contact cloud drops they cause them to
  freeze.
 Supper cold water will freeze if it impacts the ground.


                                      http://nasasport.wordpres
                                      s.com/2011/08/26/amsr-e-
                                      maps-rain-associated-
                                      with-irene/
Warm Cloud Precipitation

 When water absorbing partials remove water vapor from
  air at relative humidity.
 Salt can remove water vapor from the air.
 Tropics is an example of warm cloud Precipitation
   http://hdwallpapersdesktop.com/wallpapers/2011/08/wallpaper-ocean-tropics-clouds-boat-island-yacht-
    photo/wallpaper-ocean-tropics-clouds-boat-island-yacht-photo-2/
Rain and Snow

 Rain- drops of water that falls from clouds. Must
  be a least .5mm.
 Snow- made up of separate 6-sided crystals.
 Warmer that -5 degrees Celsius, ice crystaly join
  in large clumps.
   http://totallycoolpix.com/2011/01/us-east-coast-snow-storms/
Sleet, Glaze and Hail

 Sleet-small particles of clear-to-translucent ice.
 Glaze- Freezing rain that was freezing before hitting
    objects.
 Hail- cumulonimbus clouds ice pellets.
   http://www.erh.noaa.gov/cle/wx_events/2008/2008end.php
CLOUDS AND PRECIPITATION
         PROJECT


     By: Erinne Finlayson

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Clouds and precipitation project

  • 1. By: Erinne Finlayson CLOUDS AND PRECIPITATION PROJECT
  • 2. Adiabatic Temperature Change and Expansion and Cooling  When air expands it cools but when air is compressed it warms.  The dry adiabatic rate is when cooling and heating only affect unsaturated air.  Farther off the earths surface the less pressure.  http://www.kidsgeo.com/geography-for-kids/0070-adiabatic-temperature-changes.php
  • 3. Orographic Lifting  Mountains act like walls to air flow causing Orographic lifting.  Windward side of mountain will be rainy.  Leeward side will be dryer.  http://www.examiner.com/outdoorsman-in-salt-lake-city/understanding-why-utah-has-the- greatest-snow-on-earth-part-1-orographic-lifting
  • 4. Frontal Wedging  Cool and warm air collide producing fronts.  Cooler air is more dense than warm air.  Cool air asks like a wall against warmer air.  http://www.harding.edu/lmurray/113_files/HTML/d2_Earth%20Revised/sld0 46.htm
  • 5. Convergence  The different air masses force air to rise.  Convergence is when the lower atmosphere mix together.  Florida peninsula is a good example.  http://keithrogershome.com/Chap8Clds.html
  • 6. Localized Convective Lifting  Warmed air  Warm parcles of air rise and form condensation clouds.  May cause rain showers.  http://rst.gsfc.nasa.gov/Sect14/Sect14_1c.html
  • 7. Stability  Unstable air moves up  Stable air dose not  Unstable air= Thunderstorms maybe even tornados http://www.richho ffmanclass.com/ch apter4.html
  • 8. Condensation  Water vapor changes to liquid. (Gas to liquid)  Air must be saturated  Results in dew, fog, or clouds.  http://www.scottslumber.com/services/window- condensation-are-my-windows-defective/
  • 9. Types of Clouds  Clouds are formed by form and height.  Types  Cirrus (curl of hair) is seen as a white cloud.  Cumulus (a pile) is seen as rounded separate cloud masses. Cauliflower structure.  Stratus (a layer) seen as sheets or layers that cover most or all of the sky. http://ed101.bu.edu/StudentDoc/c urrent/ED101fa10/jenmks/
  • 10. High Clouds  Found over 6,000 meters off of earths surface.  Cirrus and Cirrostratus are two possible clouds found as a high cloud.  Warning of stormy weather coming.  http://www.zastavki.com/eng/Nature/Clouds/wallpaper-14253.htm
  • 11. Middle Clouds  Found around 2,000-6,000 meters off of earths surface.  These clouds are white or gray.  They warn of a little snow or drizzle.  http://acrosstheuniverse.forummotion.com/t862-i-ve-looked-at-clouds-from-both-sides-now
  • 12. Low Clouds  Seen as rainy clouds  Located below 2,000 meters from the Earth’s surface.  Created when air is forced up.  Stratus and Stratocumulus are some clouds that can be found here.  http://bmvgallery.com/tag/clouds/
  • 13. Clouds and Vertical Development  Made up of unstable air  These clouds cause showers and thunderstorm.  A upward movement is strong enough to give many clouds a great vertical rang form.  http://www.uwgb.edu/dutchs/EarthSC102Notes/102Clou ds.htm
  • 14. Fog  Fog and clouds are the same thing, they are just created in different place.  Fog is the cooling or movement over something cold.  Fog is found very close to the ground.  http://helicopterblog.com/?p=276
  • 15. Cold Cloud Precipitation  It the ground is 0 degrees Celsius it must be at least -40 degrees Celsius in the clouds to create snow, hail, ext.  When ice crystals contact cloud drops they cause them to freeze.  Supper cold water will freeze if it impacts the ground. http://nasasport.wordpres s.com/2011/08/26/amsr-e- maps-rain-associated- with-irene/
  • 16. Warm Cloud Precipitation  When water absorbing partials remove water vapor from air at relative humidity.  Salt can remove water vapor from the air.  Tropics is an example of warm cloud Precipitation  http://hdwallpapersdesktop.com/wallpapers/2011/08/wallpaper-ocean-tropics-clouds-boat-island-yacht- photo/wallpaper-ocean-tropics-clouds-boat-island-yacht-photo-2/
  • 17. Rain and Snow  Rain- drops of water that falls from clouds. Must be a least .5mm.  Snow- made up of separate 6-sided crystals.  Warmer that -5 degrees Celsius, ice crystaly join in large clumps.  http://totallycoolpix.com/2011/01/us-east-coast-snow-storms/
  • 18. Sleet, Glaze and Hail  Sleet-small particles of clear-to-translucent ice.  Glaze- Freezing rain that was freezing before hitting objects.  Hail- cumulonimbus clouds ice pellets.  http://www.erh.noaa.gov/cle/wx_events/2008/2008end.php
  • 19. CLOUDS AND PRECIPITATION PROJECT By: Erinne Finlayson