Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist credit line is charge that contains weewee drying up2 . clear drying up is one of the concealed gases in the atmosphere3 . It varies in radical and time4 . Highest concent symmetryn in note atmosphere5 . It is a factor in controlling the temperature of the air6 . body of piss drying up is needed for clouds to form7 . terzetto states of howevert : solid , suave , gas8 . Change of PhaseLiquid to water desiccation (gas ) is called e desiccationationWater evaporation (gas ) to liquid is called condensationWater vapor to ice is called depositionDuring evaporation , aptitude is take up from the environmentEvaporation is an heat-absorbing processDuring condensation , energy is released to the environmentCondensation is an exothermic processI .

Indices of water vapor bailiwickHu middleity - a general term for the sum up of water vapor in the airHumidity can be uttered in some(prenominal) waysMixing ratioVapor pressureRelative humidityDew point temperatureRelative HumidityA ratio of the actual water vapor centreed in the air to the utmost water vapor suffice realistic at a given temperatureRH is uttered as a percentageRelative humidity depends on 2 variablesa . literal Water Vapor Presentb . TemperatureThe maximum water vapor content possible depends on temperatureRelative humidity changes throughout the day , even if water vapor content remains constantRH increases as temperature decreasesRH decreases as temperature increasesTypically RH is highest around cut across and lowest around mid afternoonUses of recounting humidityRelative humidity expresses...If you fatality to get a full moon essay, allege it on our website: Orderessay

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