Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist ambience is air that contains body of piss dehyd dimensionn2 . 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 vapour is needed for clouds to form7 . Three states of military issue : solid , naiant , gas8 . Change of PhaseLiquid to water drying up (gas ) is called evaporationWater vapor (gas ) to liquid is called concretionWater 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 upper limit water vapor circumscribe likely at a given temperatureRH is expressed as a percentageRelative humidness depends on 2 variablesa . Actual Water Vapor Presentb . TemperatureThe maximum water vapor content possible depends on temperatureRelative humidness changes throughout the day , even if water vapor content remains constantRH increases as temperature decreasesRH decreases as temperature increas! esTypically RH is highest around get over and lowest around mid afternoonUses of relation back humidityRelative humidity expresses...If you want to get a full essay, show it on our website: BestEssayCheap.com

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