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By: Anthony Perno
   When air is compressed or allowed to expand
   When air expands it cools, when it compress it
    warms
   Dry adiabatic rate is the cooling or getting
    warmer in unsatured air
   Mountains act as barriers to air flow
   When air goes up a mountain, cooing often
    makes clouds and precipitation
   By the time the air reaches the leeward side
    most of the moisture is gone
   Warm and cold air collide, producing a front
   Cooler, denser air acts as a barrier as the
    warmer, less dense air rises
   Weather-producing fronts are associated with
    storm systems
   When air flows from more than one direction it
    flows upward because it can’t go down
   Leads to adiabatic cooling and clod formation
   Air movement and the rise of it is helped by
    solar heating of the land
   When warm air rise’s above the condensation
    level, clouds form
   Air that is warmer and less dense than the air
    around the less dense air will move upward
   The process that produces rising thermals is
    localized convective lifting
   Air that is cooler and more
    dense tends to sink to its
    original position which is stable
    air
   If the air is warmer and less
    dense than the surrounding air
    it will began to rise, this is
    called unstable air
   When stable gets forced into the
    Earth’s surface clouds that are
    formed widespread and have
    little thickness
   Happens when water vapor in the air turns
    into liquid
   For any of this to happen the air must be
    saturated
   Saturation occurs when the air is cooled to its
    dew point
   Basic form’s of
    clouds are cirrus,
    cumulus, and stratus
   Cirrus- clouds are
    high white and thin
   Cumulus- a pile of
    clouds
   Stratus- a layer of
    clouds that cover
    most of the sky
   All high clouds are thin and white
   Not considered precipitation makers
   Sometimes made up of ice crystals because low
    temperature and small amount on water vapor
    presents at high altitudes
   Clouds that are in the middle of the sky
   Altocumulus clouds are composed of rounded
    masses
   Altostratus clouds create a uniform white sheet
    covering the sky
   These clouds are developed in stable air
   Three members in the low cloud family:
    stratus, stratocumulus, and nimbostratus
   Sometimes these clouds can produce light
    precipitation
   All related to one
    another and all have
    unstable air
   Clouds have their
    bases in the low height
    range but tends to rise
    upward into the
    middle
   When clouds move
    upward and
    acceleration is
    powerful clouds with
    great vertical range
    form
   Fog is pretty much a
    cloud near or on the
    ground’s surface
   Fog can form when
    enough water vapor is
    added to the air
   When fog is dense
    enough its visibility is
    a few meters or less,
    making it hard to see
    when driving
   Cloud droplets do not freeze at 0 degrees
   Freezing nuclei can cause supercooled water to
    freeze
   Any left over water vapor becomes ice that
    lowers the relative humidity near the rest of the
    other droplets
   Some water-absorbing
    particles can remove
    water vapor from the air
    at relative humidities less
    than 100%
   When bigger water
    droplets move throw the
    air they collide with
    smaller ones
   Rainfall an be associated
    with clouds located below
    the freezing level
   Rain means drops of water falling from a cloud
   Snowflakes usually melt before they hit the
    ground and turn into rain as they fall
   There are light and fluffy snowflakes and ice
    crystals join into larger clumps to make then
    harder
   Sleet is small particles of clear ice falling from
    cloud
   Glaze is freezing rain that when raindrops
    becomes super cooled as they fall threw the air
   Hail is made in cumulonimbus clouds
THE END!!!!!!!!!!!!!!

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5aprno

  • 2. When air is compressed or allowed to expand  When air expands it cools, when it compress it warms  Dry adiabatic rate is the cooling or getting warmer in unsatured air
  • 3. Mountains act as barriers to air flow  When air goes up a mountain, cooing often makes clouds and precipitation  By the time the air reaches the leeward side most of the moisture is gone
  • 4. Warm and cold air collide, producing a front  Cooler, denser air acts as a barrier as the warmer, less dense air rises  Weather-producing fronts are associated with storm systems
  • 5. When air flows from more than one direction it flows upward because it can’t go down  Leads to adiabatic cooling and clod formation  Air movement and the rise of it is helped by solar heating of the land
  • 6. When warm air rise’s above the condensation level, clouds form  Air that is warmer and less dense than the air around the less dense air will move upward  The process that produces rising thermals is localized convective lifting
  • 7. Air that is cooler and more dense tends to sink to its original position which is stable air  If the air is warmer and less dense than the surrounding air it will began to rise, this is called unstable air  When stable gets forced into the Earth’s surface clouds that are formed widespread and have little thickness
  • 8. Happens when water vapor in the air turns into liquid  For any of this to happen the air must be saturated  Saturation occurs when the air is cooled to its dew point
  • 9. Basic form’s of clouds are cirrus, cumulus, and stratus  Cirrus- clouds are high white and thin  Cumulus- a pile of clouds  Stratus- a layer of clouds that cover most of the sky
  • 10. All high clouds are thin and white  Not considered precipitation makers  Sometimes made up of ice crystals because low temperature and small amount on water vapor presents at high altitudes
  • 11. Clouds that are in the middle of the sky  Altocumulus clouds are composed of rounded masses  Altostratus clouds create a uniform white sheet covering the sky
  • 12. These clouds are developed in stable air  Three members in the low cloud family: stratus, stratocumulus, and nimbostratus  Sometimes these clouds can produce light precipitation
  • 13. All related to one another and all have unstable air  Clouds have their bases in the low height range but tends to rise upward into the middle  When clouds move upward and acceleration is powerful clouds with great vertical range form
  • 14. Fog is pretty much a cloud near or on the ground’s surface  Fog can form when enough water vapor is added to the air  When fog is dense enough its visibility is a few meters or less, making it hard to see when driving
  • 15. Cloud droplets do not freeze at 0 degrees  Freezing nuclei can cause supercooled water to freeze  Any left over water vapor becomes ice that lowers the relative humidity near the rest of the other droplets
  • 16. Some water-absorbing particles can remove water vapor from the air at relative humidities less than 100%  When bigger water droplets move throw the air they collide with smaller ones  Rainfall an be associated with clouds located below the freezing level
  • 17. Rain means drops of water falling from a cloud  Snowflakes usually melt before they hit the ground and turn into rain as they fall  There are light and fluffy snowflakes and ice crystals join into larger clumps to make then harder
  • 18. Sleet is small particles of clear ice falling from cloud  Glaze is freezing rain that when raindrops becomes super cooled as they fall threw the air  Hail is made in cumulonimbus clouds