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Weather

AB
Weather Variablestemperature air pressure wind moisture cloud precipiation storms
TroposphereAtmosphere above earth where weather is
InsolationINcoming SOlar radiaTION
Temperatureaverage kinetic energy of particles
Isothermsmodeled by use of isolines
Sunsource of heat in atmosphere
Ways atmosphere heatedconduction from earth, isolation by gases & aerosols, long wave infrared from earth, condensation & sublimation, Coriolis wind friction
convection currentsair pressure differences, cells of winds
gas expandstemperature decreases
gas compressedtemperature increases
increased altitudetemperature decreases
decreased altitudetemperature increases
conductionheat from earth into air in atmosphere
direct absorption of insolationby gases and aerosals in atmosphere
Absorption of long wave radiationdue to water vapor, methane, carbon dioxide
condensation and sublimationdsicharge heat when clouds, fog, dew, frost form
Coriolis effect heat productionfriction where atmosphere and earth
atmospheric pressurebarometric pressure, air pressure
atmospheric pressureweith of atmosphere pushing down
barometermeasures air pressure
millibarsbarometric pressure reading
greater water vaporlower air pressure and density
lower water vaporgreater air pressure and density
greater altitudelower air pressure
lower altitudegreater air pressure and density



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