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Clouds and Precipitation Blaine Cooper

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Blaine Cooper's Clouds and Precipitation Slide Show

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Page 1: Science pp 1

Clouds and PrecipitationBlaine Cooper

Page 2: Science pp 1

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.

Page 3: Science pp 1

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.

Page 4: Science pp 1

Orographic Lifting

This is when elevated terrains act as barriers to air flow.

Page 5: Science pp 1

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.

Page 6: Science pp 1

Convergence

This is when air in the lower atmosphere flows together and causes air lifting.

Page 7: Science pp 1

Localized Convective Lifting The process when convection

warm air rises over a particular local area.

Glider pilots study these to know where to fly.

Page 8: Science pp 1

Stability

Stability resists vertical movement.

It is also a large part in the predicting of daily weather.

Page 9: Science pp 1

Condensation

This is the change of physical state of matter.

It is a change from the gaseous phase into a liquid phase.

Page 10: Science pp 1

Types of Clouds There are four types of clouds

There is the Stratus clouds

The Altostratus clouds

The Cirrus clouds

And the Cumulus clouds

Page 11: Science pp 1

High Clouds High clouds are also known as the

Cirrus clouds

They do not produce precipitation

They are the highest clouds in the atmosphere.

Page 12: Science pp 1

Medium Clouds These are the Altostratus clouds.

They have water droplets or ice crystals.

They are also very thin.

Page 13: Science pp 1

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.

Page 14: Science pp 1

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.

Page 15: Science pp 1

Fog

Liquid droplets suspended in air near surface.

Page 16: Science pp 1

Cold Cloud Precipitation This is also known as the Bergeron

process.

It is the formation of precipitation by ice crystals.

Page 17: Science pp 1

Warm Cloud Precipitation The theory of raindrop formation in

warm clouds.

Large cloud droplets collide and join together.

Known as the Collision – Coalescence process.

Page 18: Science pp 1

Rain and Snow Precipitation composed of rain and

partially melted snow.

This occurs when temperatures are slightly above freezing point.

Page 19: Science pp 1

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.