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Dan Manns
Adiabatic temperature changes
and expansion and cooling
 When temperature changes even
though there has been no changes to
the heat.
 It happens because air gets compressed
and is allowed to expand.
Orographic lifting
 Orographic lifting is when elevated land,
like mountains, act like a barrier to air
flow.
Frontal wedging
 Frontal wedging is when cooler, denser
air acts as a barrier over which the
warmer less dense air rises.
Convergence
 Convergence is whenever air in the
lower atmosphere flows together lifting
results.
Localized convective lifting
 Pockets of air being warmed more than
the surrounding air.
Stability
 If a volume of air was forced to rise, its
temperature would drop because of
expansion.
 If this volume of air was cooler than the
surrounding environment, it would be
denser, and if allowed to do so, it would
sink to its original position.
Condensation
 When water vapor in the air changes to
a liquid.
Types of clouds
 Types of clouds are based on their
shape and height
 Cirrus
 Cumulus
 Stratus
High clouds
 There are three high cloud types:
 Cirrus
 Cirrostratus
 cirrocumulus
Middle clouds
 Middle clouds are about 2,000-6,000
 All middle clouds have alto before their
name.
Low clouds
 Stratus clouds are the clouds that
usually cover most of the sky.
Sometimes they produce precipitation.
 Nimbostratus create most of the
precipitation.
Clouds of vertical development
 Clouds of vertical development have low
bases but extend upward.
Fog
 Fog is physically the same as a cloud.
 Fog is the result of radiation cooling or
the movement of air over a cold surface.
 Fog is on the ground.
Cold cloud precipitation (Bergeron
process)
 The Bergeron process relies on
supercooling and supersaturation.
 Water that is below o degrees Celsius is
supercooled.
 When air is saturated it is
supersaturated.
Warm cloud precipitation
 In warm clouds, clouds are formed by
the collision-coalescence process.
 Some water absorbing particles can
remove water vapor from the air when it
is not saturated.
Rain and snow
 Rain is a drop of water that falls from a
cloud and has a diameter of at least 0.5
mm.
 When the temperature is low, snow is
made up of six sided ice crystals.
Sleet, glaze, and hail
 Sleet is particles falling of clear ice.
 Glaze happens when raindrops become
supercold.
 Hail is smalls ice pellets.

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4dmanns

  • 2. Adiabatic temperature changes and expansion and cooling  When temperature changes even though there has been no changes to the heat.  It happens because air gets compressed and is allowed to expand.
  • 3. Orographic lifting  Orographic lifting is when elevated land, like mountains, act like a barrier to air flow.
  • 4. Frontal wedging  Frontal wedging is when cooler, denser air acts as a barrier over which the warmer less dense air rises.
  • 5. Convergence  Convergence is whenever air in the lower atmosphere flows together lifting results.
  • 6. Localized convective lifting  Pockets of air being warmed more than the surrounding air.
  • 7. Stability  If a volume of air was forced to rise, its temperature would drop because of expansion.  If this volume of air was cooler than the surrounding environment, it would be denser, and if allowed to do so, it would sink to its original position.
  • 8. Condensation  When water vapor in the air changes to a liquid.
  • 9. Types of clouds  Types of clouds are based on their shape and height  Cirrus  Cumulus  Stratus
  • 10. High clouds  There are three high cloud types:  Cirrus  Cirrostratus  cirrocumulus
  • 11. Middle clouds  Middle clouds are about 2,000-6,000  All middle clouds have alto before their name.
  • 12. Low clouds  Stratus clouds are the clouds that usually cover most of the sky. Sometimes they produce precipitation.  Nimbostratus create most of the precipitation.
  • 13. Clouds of vertical development  Clouds of vertical development have low bases but extend upward.
  • 14. Fog  Fog is physically the same as a cloud.  Fog is the result of radiation cooling or the movement of air over a cold surface.  Fog is on the ground.
  • 15. Cold cloud precipitation (Bergeron process)  The Bergeron process relies on supercooling and supersaturation.  Water that is below o degrees Celsius is supercooled.  When air is saturated it is supersaturated.
  • 16. Warm cloud precipitation  In warm clouds, clouds are formed by the collision-coalescence process.  Some water absorbing particles can remove water vapor from the air when it is not saturated.
  • 17. Rain and snow  Rain is a drop of water that falls from a cloud and has a diameter of at least 0.5 mm.  When the temperature is low, snow is made up of six sided ice crystals.
  • 18. Sleet, glaze, and hail  Sleet is particles falling of clear ice.  Glaze happens when raindrops become supercold.  Hail is smalls ice pellets.