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Precipitation Chapter 7. Objectives. Differentiate several ways that precipitation is formed Distinguish between several types of precipitation. There are several forces acting on a water droplet or ice crystal in a cloud Winds Atmospheric stability Gravity Drag (friction).
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Objectives • Differentiate several ways that precipitation is formed • Distinguish between several types of precipitation
There are several forces acting on a water droplet or ice crystal in a cloud Winds Atmospheric stability Gravity Drag (friction) When a droplet reaches a certain critical mass the force of gravity will exceed the other forces and precipitation will fall Rain drops are 100X larger than cloud droplets General concept
Formation of precipitation • Condensation and deposition • Collision and coalescence • The Bergeron process Warm air Cold air
Condensation and deposition • As long as the rate of condensation exceeds the rate of evaporation water will be deposited and accumulate on condensation nuclei • Droplets grow very slowly • Rarely produces rain drops
Collision and coalescence • As water droplets fall through a cloud, the larger droplets fall faster than the smaller ones, thus they collide • If the droplets coalesce a larger drop is formed • If it gets big enough rain will fall
Collision efficiency A drop must be larger than the other drops to be an efficient collider If the drop is too big it will be less efficient, because it creates high pressure that pushes small drops out of the way
Cold < 00C throughout Cool Part is < 00C Part is > 00C Cold and cool clouds
The Bergeron process Vapor pressure over ice is less than vapor pressure over water of the same temperature Thus, water molecules move from water to ice and freeze on the ice If the crystals get large enough they will fall If they fall through cold air they will stay frozen and it will snow If they fall through warm air they will melt and it will rain
Riming – super-cooled water freezes onto ice crystals Aggregation – Ice crystals join together to form large snow flakes. Happens more readily if ice crystals have a thin coating of liquid Growth of ice crystals
Types of precipitation rain sleet graupel hail freezing rain
Rain Can originate as liquid drops or ice. Ice melts as it falls through warmer air Shape of rain drops
Snow • Ice crystals grow in a cloud. Variety of shapes depending on temperature
Graupel • Ice crystals grow by riming • Contain air pockets • Has a spongy texture
Sleet • Ice crystals melt as they fall through warn air aloft. Then water drops freeze as they fall through cold air below and hit the surface as ice pellets
Freezing Rain • Ice crystals fall through warm air aloft and melt, Then liquid water falls through air at nearly 00C and freezes when it hits the cold (00C)ground
Hail • Strong updrafts in a cloud force ice particles upward • As they move up and down in the cloud hail stones accumulate layers of ice • Eventually they get too heavy and fall