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Heating the Atmosphere

AB
conductiondirect physical contact
convectionhot air rises, cold air sinks
radiationhow sun's energy reaches us
equatorlatitude with most constant length of day light
90 degreeslatitudes with the longest lenght of day light
insolationhow much solar energy strikes a given area
concentrateddescribes energy when sun's rays strike straight on
large illuminated areadescribes area where sun's rays strike at an angle
smogconbination of pollution and fog
absorptionenergy is soaked up
reflectionenergy is bounced back
albedomeasure of how much light is reflected
waterhas a high albedo
dark soilhas a low albedo


Laura Sheaffer

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