Atmospheric Science

Atmospheric MoistureChapter 5I . Review1 . Moist air is air that contains weewee drying up2 . urine drying up is one of the invisible gases in the atmosphere3 . It varies in al-Qaida 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 . ternion states of level offt : solid , liquid , gas8 . Change of PhaseLiquid to water dehydrationization (gas ) is called evaporationWater vapor (gas ) to liquid is called condensationWater vapor to ice is called depositionDuring evaporation , vigour 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 bailiwickHu middleity - a general term for the bill of water vapor in the airHumidity can be denotative in some(prenominal) waysMixing ratioVapor pressureRelative humidityDew point temperatureRelative HumidityA ratio of the actual water vapor bailiwicked in the air to the maximum water vapor content realistic at a given temperatureRH is verbalized as a percentageRelative humidity depends on 2 variablesa . true(a) 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 decrease sRH decreases as temperature increasesTypica! lly RH is highest around dawn and lowest around mid afternoonUses of recounting humidityRelative humidity expresses...If you want to get a wax essay, allege it on our website: BestEssayCheap.com

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