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Physical Geography CH 7

Water and Atmospheric Moisture

AB
2 Ways air coolsWinds Lift Air Up; Adiabatic heating/cooling
DARDry Adiabatic Rate
MARMoist Adiabatic Rate
Adiabatic ChangeChange in Temperature due ONLY to a change in pressure
fogground cloud
3 types of FogAdvection; Evaporation Fog; Radiation Fog
Advection FogWarm air moving over cooler ground
Evaporation FogCold air moving over warm ground
Radiation FogRapid Temp Drop - clear night Heat radiates back to atmosphere
2 Critera of CloudsAltitude and shape
Cloud AltitudeLow (Below 2000m); Middle (2000-6000m); High (Above 60000m)
Cloud ShapesStratus; Cumulus; Cirrus
Cumulonimbusclouds with vertical development
Stratuslayered clouds
CumulusPuffy clouds like cotton balls
CirrusWispy clouds (usually ice crystals)
Production of RainTemp decrease to Dew Point; RH-100%; Condensation; Clouds; Collision-Coalescence; Heavy Drops of Water; Rain
RainWhen water molecules accumulate and weigh more than atmosphere
as temp clouds dropspeed will drop
cloud temperatureheat energy determines how fast they collide and stick together
Dew PointTemperature at which relative humidity reaches 100%.
How high can R.H. go100%
SATURATIONCANNOT HOLD ANY MORE MOISURE AND THE MOISTURE CONDENSES BACK TO A LIQUID STATE
clouds develop becausewater has been squeezed out of the air.
Relative Humidity goes upwhen air temperature gets colder
Relative Humidity goes downwhen air temperature gets warmer
relational humidity= relative humidity
humidity% of water vapor in the air
relative humiditymaximum amount of water vapor the air can hold
Unique Properties of Water3 Phases; Heat in/out; Cohesion; Solvent
3 Phases of watersolid-ice; liquid-water; gas-water vapor (steam)
Boiling point of water100 degrees celcius
Cohesionpolarity of water produces a hydrogen bond
Solventwater dissolves most materials
sublimation(+ or -) solid to gas or gas to solid


Olathe, KS

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