Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist mien is air that contains body of weewee dehyd symmetryn2 . 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 e evaporationation is needed for clouds to form7 . Three states of military issue : solid , liquid , gas8 . Change of PhaseLiquid to water vapor (gas ) is called evaporationWater vapor (gas ) to liquid is called compactionWater 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 humidityDew point temperatureRelative HumidityA ratio of the actual water vapor capability in the air to the utmost water vapor issue 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 increase s as temperature decreasesRH decreases as te! mperature increasesTypically RH is highest around filter 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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