chapter 4 Flashcards
water vapor
transforms into cloud droplets and ice crystals
humidity
amount of water vapor in the air, not constant through time and space
Evaporation
energy from the sun transforms enormous quantities of liquid water into water vapor
condensation
water vapor changes back into liquid, forming clouds
precipitation
rain, snow, or hail
water cycle
Evaportation -> condensation->
precipitation
saturation
total number of molecules escaping from evaporation are balanced by the number condensing
Humidity
specific amount of water vapor in the air
absolute humidity
mass of water vapor compared with the volume of air
specific humidity \
mass of water vapor compared with the mass of air
mixing ratio
mass of water vapor compared to with the mass of dry air
actual vapor pressure
partial pressure of water vapor
saturation vapor pressure
amount of water vapor necessary to make the air saturated at any given temperature
partial pressure
the part of the total pressure exerted by just one component
Relative humidity
ratio of water vapor in air to maximum amount of water vapor requird for saturation at that particular temperature
Ways to change relative humidity?
increase water vapor -> increased relative humidity
decreased temperature -> increased relative humidity
Dew point
the temp at which saturation occurs
psychrometer
two liquid in glass thermometers mounted side by side and attached to a piece of metal that has either a handle or chain at on end
hygrometer
hair hygrometer
How is frost formed?
when dew point is at or below freezing
Haze
layers of particles dispersed through a portion of the atmosphere
fog
cloud resting near the ground when visibility lowers to less than 1 km
radiation fog
earth cools and the temperature drops to the dew point, causing water to condense out of the air
advection fog
warm, moist air moves over a colder surface(air coming off an ocean)