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Blaine Cooper's Clouds and Precipitation Slide ShowTRANSCRIPT
Clouds and PrecipitationBlaine Cooper
Adiabatic Temperature Changes
This is when the temperature changes but heat is not added or subtracted.
This happens because air is compressed or allowed to expand.
Expansion and Cooling Unsaturated air cools at a rate of
10 degrees Celsius for every 1,000 meters of ascent.
This also works vise versa.
Orographic Lifting
This is when elevated terrains act as barriers to air flow.
Frontal Wedging 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.
Convergence
This is when air in the lower atmosphere flows together and causes air lifting.
Localized Convective Lifting The process when convection
warm air rises over a particular local area.
Glider pilots study these to know where to fly.
Stability
Stability resists vertical movement.
It is also a large part in the predicting of daily weather.
Condensation
This is the change of physical state of matter.
It is a change from the gaseous phase into a liquid phase.
Types of Clouds There are four types of clouds
There is the Stratus clouds
The Altostratus clouds
The Cirrus clouds
And the Cumulus clouds
High Clouds High clouds are also known as the
Cirrus clouds
They do not produce precipitation
They are the highest clouds in the atmosphere.
Medium Clouds These are the Altostratus clouds.
They have water droplets or ice crystals.
They are also very thin.
Low Clouds 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.
Clouds of Vertical Development
The vertical clouds are Cumulus.
These clouds look puffy and cotton like.
They are also associated with hail, waterspouts, and tornadoes.
Fog
Liquid droplets suspended in air near surface.
Cold Cloud Precipitation This is also known as the Bergeron
process.
It is the formation of precipitation by ice crystals.
Warm Cloud Precipitation The theory of raindrop formation in
warm clouds.
Large cloud droplets collide and join together.
Known as the Collision – Coalescence process.
Rain and Snow Precipitation composed of rain and
partially melted snow.
This occurs when temperatures are slightly above freezing point.
Sleet, Glaze, and Hail Could occur in an ice storm, freezing
rain, and/ or glaze event.
This can occur only when temperatures are below the freezing point.