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Roland-Story Meteorology Chapter 4 -- Matching

Chapter 4 -- Moisture and the atmosphere

AB
absolute instabilitythe condition of air that has an enviromental lapse rate that is greater than the dry abiabatic rate
wet adiabatic ratethe rate of adiabatic temperature change in saturated air
absolute stabilitythe condition of air that has an enviromental lapse rate that is less than the wet abiabatic rate
adiabatic temperaturethe cooling or warming of air caused when air is allowed to expand or contract and not due to heat
condensationis the change of the physical state of aggregation of matter from gaseous phase into liquid phase
convergencethe approach toward a definite value
depositionthe process of gas transformation into solid
dewpointis the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water.
dry adiabatic ratethe rate of adiabatic cooling or warming in unsaturated air
entrainmenta phenomenon of the atmosphere
evaporationis the process by which molecules in a liquid state become gaseous
frontal wedgingthe lifing of air resulting when cool air acts as a barrier over which warmer, lighter air will rise
humidityis the amount of water vapor in the air
hydrologic cyclethe continuous movement of water on, above, and below the surface of the Earth
hygrometerinstruments used for measuring humidity
latent heatis the amount of energy in the form of heat released or absorbed by a substance during a change of phase
mixing ratiothe mass or water vapor in a unit mass of dry air
orographictype of lifting that occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain
relative humidityis a term used to describe the amount of water vapor that exists in a gaseous mixture of air and water.
saturation pointis the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water
psychrometerinstrument on a sling used to measure humidity in the air
stable airair that resists vertical displacement
sublimationthe change from solid to gas, while at no point becoming a liquid.
transpirationis the evaporation of water from plants
unstable airair that does not resist vertical displacement
vapor pressureis the pressure of a vapor in equilibrium with its non-vapor phases
absolute humidityis the quantity of water in a particular volume of air



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