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   This is when the temperature changes but
    heat is not added or subtracted.

   This happens because air is compressed or
    allowed to expand.
 Unsaturated   air cools at a rate of
  10 degrees Celsius for every 1,000
  meters of ascent.
 This also works vise versa.
This  is when elevated
 terrains act as barriers to
 air flow.
 In central North America warm air
  masses and cold collide, producing a
  front.
 The cooler, denser air acts as a barrier
  over which the warmer, less dense air
  rises.
This  is when air in the
 lower atmosphere flows
 together and causes air
 lifting.
 The process when convection
  warm air rises over a particular
  local area.
 Glider pilots study these to know
  where to fly.
 Stability  resists vertical
  movement.
 It is also a large part in the
  predicting of daily weather.
 This  is the change of physical
  state of matter.
 It is a change from the
  gaseous phase into a liquid
  phase.
   There are four types of clouds

   There is the Stratus clouds

   The Altostratus clouds

   The Cirrus clouds

   And the Cumulus clouds
   High clouds are also known as the Cirrus
    clouds

   They do not produce precipitation

   They are the highest clouds in the
    atmosphere.
   These are the Altostratus clouds.

   They have water droplets or ice crystals.

   They are also very thin.
   The low clouds are the Stratus clouds

   They produce a light drizzle or snow

   They are the lowest in the atmosphere,
    and are known to be flat.
   The vertical clouds are Cumulus.

   These clouds look puffy and cotton like.

   They are also associated with hail,
    waterspouts, and tornadoes.
Liquid droplets
 suspended in air near
 surface.
   This is also known as the Bergeron
    process.

   It is the formation of precipitation by ice
    crystals.
   The theory of raindrop formation in warm
    clouds.

   Large cloud droplets collide and join
    together.

   Known as the Collision – Coalescence
    process.
   Precipitation composed of rain and
    partially melted snow.

   This occurs when temperatures are
    slightly above freezing point.
   Could occur in an ice storm, freezing
    rain, and/ or glaze event.

   This can occur only when temperatures
    are below the freezing point.

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Science pp 1

  • 1.
  • 2. This is when the temperature changes but heat is not added or subtracted.  This happens because air is compressed or allowed to expand.
  • 3.  Unsaturated air cools at a rate of 10 degrees Celsius for every 1,000 meters of ascent.  This also works vise versa.
  • 4. This is when elevated terrains act as barriers to air flow.
  • 5.  In central North America warm air masses and cold collide, producing a front.  The cooler, denser air acts as a barrier over which the warmer, less dense air rises.
  • 6. This is when air in the lower atmosphere flows together and causes air lifting.
  • 7.  The process when convection warm air rises over a particular local area.  Glider pilots study these to know where to fly.
  • 8.  Stability resists vertical movement.  It is also a large part in the predicting of daily weather.
  • 9.  This is the change of physical state of matter.  It is a change from the gaseous phase into a liquid phase.
  • 10. There are four types of clouds  There is the Stratus clouds  The Altostratus clouds  The Cirrus clouds  And the Cumulus clouds
  • 11. High clouds are also known as the Cirrus clouds  They do not produce precipitation  They are the highest clouds in the atmosphere.
  • 12. These are the Altostratus clouds.  They have water droplets or ice crystals.  They are also very thin.
  • 13. The low clouds are the Stratus clouds  They produce a light drizzle or snow  They are the lowest in the atmosphere, and are known to be flat.
  • 14. The vertical clouds are Cumulus.  These clouds look puffy and cotton like.  They are also associated with hail, waterspouts, and tornadoes.
  • 15. Liquid droplets suspended in air near surface.
  • 16. This is also known as the Bergeron process.  It is the formation of precipitation by ice crystals.
  • 17. The theory of raindrop formation in warm clouds.  Large cloud droplets collide and join together.  Known as the Collision – Coalescence process.
  • 18. Precipitation composed of rain and partially melted snow.  This occurs when temperatures are slightly above freezing point.
  • 19. Could occur in an ice storm, freezing rain, and/ or glaze event.  This can occur only when temperatures are below the freezing point.