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radiation
waves of energy traveling through open space
conduction
energy transfer when an object comes in contact with another object
convection
energy transfer via currents in liquids and gases created by the rise and fall due to temperature differences
insolation
radiation from sun
albedo
average percent reflected back toward space - reflectivity
greenhouse effect
thick gasses trap radiation from escaping back into space the energy waves from the sun are short while waves from surface are long
adiabatic heating/cooling
temperature changes caused by pressure changes
temperature inversion
layer of warmer air sits over a layer of cooler denser air near ground
troposphere
lowest layer where all weather takes place
stratosphere
contains the ozone layer which protects earth’s surface from being bombarded with too much harmful radiation
cfc
causing stratospheric ozone depletion and driving global warming
ozone
03 highly reactive gas composed of 3 oxygen atoms
specific humidity
actual amount of water vapor in the air
relative humidity
comparison between actual and capacity
dew point
temp to which air must be cooled at constant pressure and moisture to be fully saturated with water vapor
condensation nuclei
microscopic atmospheric particles that serves as surfaces for water vapor to condense into liquid droplets
orographic lifting
one side of mountain is wetter than the other
coriolis effect
curving of moving objects due to earth’s rotation