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30 Cards in this Set
- Front
- Back
Describig a change in temperature resulting from the cooling of rising air and the warming of sinking air.
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Adiabatic
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Condensation of water vapor that results from the coolig of warm, moist air as it moves across a cold surface.
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Advection Fog
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Decrease in the temperature of a mass of air that results as it moves over a cold surface.
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Advective Cooling
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Feathery cloud composed of ice crystals that has the highest altitude of any cloud in the sky.
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Cirrus Coud
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Addition of freezing nuclei to supercooled clouds in an attempt to induce or increase precipitation.
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Cloud Seeding
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Combination of different sized cloud droplets to form larger droplets.
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Coalescence
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Solid particles in the atmosphere, such as ice and dust,that provide the surfaces on which water vapor condenses.
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Condensation Nuclei
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Decrease in the temperature of a mass of air that results as the air rises and expands.
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Convective Cooling
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Thick, billowy cloud that forms above stratus clouds and below cirrus clouds.
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Cumulus Cloud
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Type of condensation formed when air that is in contact with a cool surface loses heat until it reaches saturation.
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Dew
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Temperature to which air must be cooled to become saturated.
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Dew Point
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Condensation nuclei with a crystalline structure like that of ice.
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Freezing Nuclei
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Ice crystals formed when the dew point is below 0 degrees C and water vapor directly enters the solid state.
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Frost
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Thick layer of sheet ice formed when rain freezes as it contacts a surface.
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Glaze Ice
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Type of precipitation in the form of lumps of ice.
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Hail
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Instrument used to measure relative humidity, based on the fact that human hair stretches as humidity increases.
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Hair Hygrometer
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Amount of water vapor in the atmosphere.
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Humidity
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Energy stored in molecules.
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Latent Heat
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Instrument used to measure relative humidity.
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Psychrometer
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Condensation of water vapor that results from the cooling of air that is in contact with the ground.
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Radiation Fog
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Instrument used to measure the amount of rainfall.
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Rain Gauge
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Ratio of the amount of water vapor in the air to the amount of water vapor the air can hold when saturated.
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Relative Humidity
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Describing air that contains all the water vapor it can hold at a specifc temperature.
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Saturated
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Ice pellets that form when rain falls through a layer of freezing air.
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Sleet
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Actual amount of moisture in the air.
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Specific Humidity
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Condensation of water vapor that results when cool air moes over warm water.
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Steam Fog
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Cloud with a sheetlike or layered form that is the lowest cloud in the sky.
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Stratus Cloud
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Process in which a solid changes directly into a gas, or a gas changes directly into a solid.
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Sublimation
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Process in which water droplets are induced to remain liquid at temperatures below 0 degrees C.
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Supercooling
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Condensation of wayer vapor that results from the lifting and adiabatic cooling of air rising up a slope of land.
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Upslope Fog
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