9/28/2009 Electromagnetic Spectrum Energy and the Atmosphere Radio Microwaves IR Visible UV X-rays Gamma Short LONG Wavelength ~ different colors Visible light – White light Solar Energy Scattering Cause of color of sky and clouds Reflection (Albedo) Determines amount of energy reflected away from an object. High albedo light colors Low albedo dark colors Absorption of Solar Energy Sun heats the land… …Land heats the air. Absorption of Solar Energy Land Solar energy absorbed at different times of day and at different latitudes Direct sun angle at tropics Direct sun angle mid-day Indirect sun at poles Indirect sun at morning/evening Atmosphere O3 in Stratosphere absorbs UV Short wavelength that reaches surface may cause sunburn CO2 absorbs IR (also H2O and CH4) Mistakenly referred to as Greenhouse effect. 1 9/28/2009 Transfer of Energy Conduction Energy transfer from atom to atom (often in solids) Convection Energy transfer in liquid or gas Density and Gravity • Warm substance less dense (floats) • Cold more dense (sinks) ***Measurement of Energy Temperature – The measurement of atomic movement. 2
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