Ch.4 : humidity,Condensation, Clouds Flashcards
Condensation
water vapor changes back to liquid
evaporation
sun’s energy transforms enormous quantities of liqiud into water vapor
saturation
condensation & evaporation are equal humidity is now 100% = same # of water leavin the liquid as going back in
for every molecule that evaporates , one musy condense
subsaturation
if more evaporation is occurring than condensation, then net evaporation is occurring
supersaturation
if more condensation than evaporation is occurring
cloud condensation nuclei
air molecules are microscopic bits of dust, smoke and salt, many of these surfaces on which water spray condense
humidity
refers to any one of a number of specifying the amount of water vapor in air
relative humidity
•ratio of the amount of water vapor actually in the air to maximum amount of water vapor required for saturation at a particular temp & pressure
• its ratio of airs water vapor content to its capacity
R.H = water vapor content/ water vapor capacy
vapor pressure
the partial pressure of water vapor
saturation vapor pressure
how much water vapor is necessary to make the air saturated at any given temperature
dew point
•represents the temp to which air would have to be cooled (with no chamge in air pressure or moisture content) for saturation to occur
•good indicator of the air’s actual water vapor content
•high dew points indicate high water vapor content
low dew point = low water vapor content
dew
as surface cools below this temp , water vapor begins to condense upon them , forming tiny visible soecks of water
frost
delicate white crystals of ice that form in this manner
fog
when visibility lowers to less than 1 km & air is west with millions of tiny droplets, the haze becomes a cloud resting near the ground
cloud
visible aggregate of tiny water droplets or ice crystals suspended in the air