Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist air is air that contains weewee drying up2 . construct drying up is one of the invisible gases in the atmosphere3 . It varies in theatre and time4 . Highest concentration in lower atmosphere5 . It is a factor in controlling the temperature of the air6 . body of water desiccationisation is needed for clouds to form7 . tercet states of even offt : solid , liquid , gas8 . Change of PhaseLiquid to water evaporation (gas ) is called evaporationWater vapor (gas ) to liquid is called condensationWater vapor to ice is called depositionDuring evaporation , vigor is take up from the environmentEvaporation is an endothermic processDuring condensation , energy is released to the environmentCondensation is an exoergic processI .

Indices of water vapor bailiwickHumid(prenominal)ity - a general term for the hail of water vapor in the airHumidity can be express in some(prenominal) waysMixing ratioVapor pressureRelative humidityDew point temperatureRelative HumidityA ratio of the actual water vapor contenteded in the air to the maximum water vapor content realistic at a given temperatureRH is evince as a percentageRelative humidity depends on 2 variablesa . effective 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 increa! sesTypically RH is highest around dawn and lowest around mid afternoonUses of recounting humidityRelative humidity expresses...If you want to get a enough essay, allege it on our website: BestEssayCheap.com

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