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ch 15 voc

AB
HumidityThe general term for the amount of water vapor in the air
CondensationCondensation The process whereby water vapor changes to the liquid state
Relative humidityThe ratio of the air’s actual water vapor content to its potential water vapor capacity at a given temperature
Orographic liftingA result of elevated terrains, such as mountains acting as barriers to flowing air
Vapor pressureThe part of total atmospheric pressure attributable to water vapor content
Adiabatic temperature changeA result of air being compressed or allowed to expand
Latent heatThe energy stored or released during a change of state
CloudVisible aggregates of minute water droplets or tiny crystals of ice suspended in the air
SleetSleet Frozen or semifrozen rain formed when raindrops freeze as they pass through a layer of cold air
SaturationThe term that refers to the maximum possible quantity of water vapor that air can hold at any given temperature and pressure
Wet adiabatic rateThe rate of adiabatic temperature change in saturated air
SublimationThe conversion of a solid directly to a gas without passing though the liquid state
StratusStratus Sheets or layers of clouds that cover much or all of the sky
Specific humidityThe weight of water vapor per weight of a chosen mass of air including the water vapor
Frontal wedgingOccurs when cool air acts as a barrier over which warmer, less dense air rises.
Condensation nucleiIn the atmosphere, tiny bits of particulate matter which serve as surfaces for water vapor condensation
MeltingThe process by which a solid is changed to a liquid
RainIn meteorology, the falling of water drops from a cloud with diameters > 0.5 mm
Dew pointThe temperature to which air would have to be cooled to reach saturation
RimeThe deposit of ice crystals formed by the freezing of supercooled fog or cloud droplets on objects whose surface temperature is below freezing
DepositionThe conversion of vapor directly to a solid
HailNearly spherical ice pellets which have concentric layers and are formed by the successive freezing of layers of water
Dry adiabatic rateThe adiabatic rate of cooling or heating which applies only to unsaturated air
Hygroscopic nucleiWater absorbing particles, such as salt
EvaporationThe process of converting a liquid to a gas
Radiation fogThe type of fog that forms on coo., clear, calm nights, when Earth’s surface cools rapidly by radiation
FogThe type of fog that forms on coo., clear, calm nights, when Earth’s surface cools rapidly by radiation
Rainshadow desertA dry area on the lee side of a mountain that forms as air descends and is warmed by compression
CirrusHigh, thin, and delicate clouds
ConvergenceOccurs whenever air masses flow together
CalorieThe common unit of heat energy , the amount of heat required to raise the temperature of 1 gram of water 1 degree C
SupercooledWater in the liquid state below ) degrees C
hygrometerAn instrument used to measure relative humidity

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