By: Jorge Rodriguez
   When temperature is changing even though
    heat isn't being given or taken away
   When air expands it cools and when air is
    compressed it gets warm, when this happens
    this is called dry adiabatic rate
   When cooling is at a slower rate because of heat
    is being added it is called wet adiabatic
   Mountains act as barriers to air flow
        As air goes up the mountain slope adiabatic
         cooling begins to make clouds and
         precipitation
        When the air reaches the leeward side of he
         mountain most of its moisture has been lost
         and condensation and precipitation is less
         likely to happen
http://www.sci.uidaho.edu/script
er/geog100/lect/05-atmos-water-
wx/05-part-7-atmos-lifting-
fronts/ch5-part-7a-atmos-liftin.htm
   When masses of warm air and cold air collide
    producing a front
   Cool denser air act as a barrier over the less
    denser air.
   Weather producing fronts are associated with
    specific storm systems which is called middle
    latitude cyclones
   When air flows in from more than one
    direction it begins to flow upward because it
    cant go down
   Causes cloud development and precipitation
   Air movement and the rise of it is helped by
    solar heating of the land
   When the volume of air was forced to rise, its
    temperature will drop because of its expansion
   The warm air that is less dense in its surrounding air,
    will keep going upward until it reaches a altitude
    where its temperature equals its surrounding air
   When stable air is moved above the earth surface, the
    clouds that form are widespread and have little
    vertical thickness.
   When water vapor in the air changes to a liquid
   When condensation happens in the air above
    the ground, tiny bits of particulate matter
    called condensation nuclei are used as a surface
    for water vapor condensation
   When condensation happens the growth rate of
    cloud droplets is very rapid
   All clouds are one of these basic forms: cirrus, cumulus
    and stratus
   Cirrus clouds are high white and thin, they have a
    feathery appearance also occur as delicate veil like
    sheets
   Cumulus clouds normally have a flat base and look like
    rising domes or towers, they clouds are describe of
    having a cauliflower structure
   Stratus clouds are layers that cover up most of the sky
   Normally have a bases of 6000 meters
   Three could types make up the family of the
    high clouds, cirrus, cirrostratus and
    cirrocumulus
   All high clouds are thin and white and are
    often made up of crystal ice
   High clouds are not consider precipitation
    makers
   Middle clouds occupy heights from 2000 to
    6000 meters, have the prefix alto in their name
   Altocumulus clouds are larger and denser than
    cirrocumulus clouds
   Altostratus clouds a white and grayish sheet
    covering the sky with the sun or moon
   Light snow or drizzle may accompany these
    clouds
   Low clouds form below 2000 meters
   there are three members of the low cloud family they
    are stratus, stratocumulus and nimbostratus
   Stratus clouds are a fog like layers of clouds the cover
    up most of the sky
   Stratocumulus clouds are when stratus clouds create a
    scalloped bottom that appear long parallel rolls
   Nimbostratus clouds form during stable air, this cloud
    is one of the main precipitation makers
   These clouds aren’t in any of the other three
    height categories, they are in the low height
    range
   Often extend to middle or high altitude
   They are all related to unstable air except the
    cumulus cloud, that is connected to fair
    weather
   Fogs are the result of radiation cooling or the
    movement of air over a cooled surface
   Fogs can also form by cool air because of the
    earth surface cools rapidly by radiation
   Fog also is caused by evaporation because
    when rising water vapor meets cold air it
    begins to condense and rise with the air that is
    being warmed from below
   The bergeron process relies on two physical
    process which is super cooling and
    supersaturated
   Super cooling is when water is in the liquid
    state but under 0 degrees Celsius
   Supersaturated is when air is 100 percent
    relative humidity
   salt the water absorbing particle can remove
    water vapor from the air even if the relative
    humidity is less than 100 percent
   Large water droplets form the humidity that is
    being taken away as these droplets move
    through the clouds they begin to collide
   The term rain means water that falls from
    clouds and that a diameter of .5 mm
   When temperature is above 4 degrees Celsius
    snow flakes will melt and turn into rain before
    they hit the ground
   When temperatures are warmer than -5
    degrees Celsius ice crystals join together a
    become bigger clumps
   Sleet is small particles of clear translucent that form
    from temperatures above freezing overlie a
    subfreezing ground
   Glaze is also known as freezing rain but they form
    when rain drops become super cold as they fall
    through subfreezing air
   Hail is produced in the cumulonimbus cloud they are
    in the shape of small ice pellets that grow as they
    collect super cooled rain drops

5jrodriguez

  • 1.
  • 2.
    When temperature is changing even though heat isn't being given or taken away  When air expands it cools and when air is compressed it gets warm, when this happens this is called dry adiabatic rate  When cooling is at a slower rate because of heat is being added it is called wet adiabatic
  • 3.
    Mountains act as barriers to air flow  As air goes up the mountain slope adiabatic cooling begins to make clouds and precipitation  When the air reaches the leeward side of he mountain most of its moisture has been lost and condensation and precipitation is less likely to happen http://www.sci.uidaho.edu/script er/geog100/lect/05-atmos-water- wx/05-part-7-atmos-lifting- fronts/ch5-part-7a-atmos-liftin.htm
  • 4.
    When masses of warm air and cold air collide producing a front  Cool denser air act as a barrier over the less denser air.  Weather producing fronts are associated with specific storm systems which is called middle latitude cyclones
  • 5.
    When air flows in from more than one direction it begins to flow upward because it cant go down  Causes cloud development and precipitation  Air movement and the rise of it is helped by solar heating of the land
  • 6.
    When the volume of air was forced to rise, its temperature will drop because of its expansion  The warm air that is less dense in its surrounding air, will keep going upward until it reaches a altitude where its temperature equals its surrounding air  When stable air is moved above the earth surface, the clouds that form are widespread and have little vertical thickness.
  • 7.
    When water vapor in the air changes to a liquid  When condensation happens in the air above the ground, tiny bits of particulate matter called condensation nuclei are used as a surface for water vapor condensation  When condensation happens the growth rate of cloud droplets is very rapid
  • 8.
    All clouds are one of these basic forms: cirrus, cumulus and stratus  Cirrus clouds are high white and thin, they have a feathery appearance also occur as delicate veil like sheets  Cumulus clouds normally have a flat base and look like rising domes or towers, they clouds are describe of having a cauliflower structure  Stratus clouds are layers that cover up most of the sky
  • 9.
    Normally have a bases of 6000 meters  Three could types make up the family of the high clouds, cirrus, cirrostratus and cirrocumulus  All high clouds are thin and white and are often made up of crystal ice  High clouds are not consider precipitation makers
  • 10.
    Middle clouds occupy heights from 2000 to 6000 meters, have the prefix alto in their name  Altocumulus clouds are larger and denser than cirrocumulus clouds  Altostratus clouds a white and grayish sheet covering the sky with the sun or moon  Light snow or drizzle may accompany these clouds
  • 11.
    Low clouds form below 2000 meters  there are three members of the low cloud family they are stratus, stratocumulus and nimbostratus  Stratus clouds are a fog like layers of clouds the cover up most of the sky  Stratocumulus clouds are when stratus clouds create a scalloped bottom that appear long parallel rolls  Nimbostratus clouds form during stable air, this cloud is one of the main precipitation makers
  • 12.
    These clouds aren’t in any of the other three height categories, they are in the low height range  Often extend to middle or high altitude  They are all related to unstable air except the cumulus cloud, that is connected to fair weather
  • 13.
    Fogs are the result of radiation cooling or the movement of air over a cooled surface  Fogs can also form by cool air because of the earth surface cools rapidly by radiation  Fog also is caused by evaporation because when rising water vapor meets cold air it begins to condense and rise with the air that is being warmed from below
  • 14.
    The bergeron process relies on two physical process which is super cooling and supersaturated  Super cooling is when water is in the liquid state but under 0 degrees Celsius  Supersaturated is when air is 100 percent relative humidity
  • 15.
    salt the water absorbing particle can remove water vapor from the air even if the relative humidity is less than 100 percent  Large water droplets form the humidity that is being taken away as these droplets move through the clouds they begin to collide
  • 16.
    The term rain means water that falls from clouds and that a diameter of .5 mm  When temperature is above 4 degrees Celsius snow flakes will melt and turn into rain before they hit the ground  When temperatures are warmer than -5 degrees Celsius ice crystals join together a become bigger clumps
  • 17.
    Sleet is small particles of clear translucent that form from temperatures above freezing overlie a subfreezing ground  Glaze is also known as freezing rain but they form when rain drops become super cold as they fall through subfreezing air  Hail is produced in the cumulonimbus cloud they are in the shape of small ice pellets that grow as they collect super cooled rain drops