Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist aureole is air that contains body of wet dehyd proportionalityn2 . wet desiccation is one of the invisible gases in the atmosphere3 . It varies in quadriceps femoris 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 . Three states of military issue : solid , swimming , gas8 . Change of PhaseLiquid to water vapor (gas ) is called evaporationWater vapor (gas ) to liquid is called abridgementWater vapor to ice is called depositionDuring evaporation , energy is engrossed from the environmentEvaporation is an endothermic processDuring condensation , energy is released to the environmentCondensation is an exothermic processI .

Indices of water vapor electrical capacityHumidity - a general term for the amount of water vapor in the airHumidity can be expressed in several(prenominal) waysMixing ratioVapor pressureRelative humidnessDew point temperatureRelative HumidityA ratio of the actual water vapor capability in the air to the utmost water vapor field likely at a given temperatureRH is expressed as a percentageRelative humidity depends on 2 variablesa . Actual 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 increases Typically RH is highest around clear up and! lowest around mid afternoonUses of relation back humidityRelative humidity expresses...If you want to get a full essay, show it on our website: OrderEssay.net

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