Exam 6: Stability and Cloud Development
Exam 1: Earth and Its Atmosphere100 Questions
Exam 2: Energy - Warming the Earth and the Atmosphere100 Questions
Exam 3: Seasonal and Daily Temperatures99 Questions
Exam 4: Atmospheric Humidity100 Questions
Exam 5: Condensation - Dew - Fog - and Clouds100 Questions
Exam 6: Stability and Cloud Development100 Questions
Exam 7: Precipitation100 Questions
Exam 8: Air Pressure and Winds100 Questions
Exam 9: Wind - Small-Scale and Local Systems99 Questions
Exam 10: Wind - Global Systems100 Questions
Exam 11: Air Masses and Fronts100 Questions
Exam 12: Middle Latitude Cyclones100 Questions
Exam 13: Weather Forecasting100 Questions
Exam 14: Thunderstorms100 Questions
Exam 15: Tornadoes100 Questions
Exam 16: Hurricanes100 Questions
Exam 17: Earths Changing Climate100 Questions
Exam 18: Global Climate100 Questions
Exam 19: Air Pollution100 Questions
Exam 20: Light - Color and Atmospheric Optics100 Questions
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It is possible for a layer of air to be convectively unstable and absolutely stable at the same time.
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True
If an air parcel is given a small push upward and it continues to move upward on its own accord, the atmosphere is said to be dynamic.
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B
List and explain several processes by which a stable atmosphere can be made unstable.
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The atmosphere becomes more unstable as the environmental lapse rate steepens; that is, as the air temperature drops rapidly with increasing height. This circumstance may be brought on by either air aloft becoming colder or the surface air becoming warmer. The cooling of the air aloft may be due to winds bringing in colder air (cold advection), and clouds (or the air) emitting infrared radiation to space (radiational cooling). The warming of the surface air may be due to daytime solar heating of the surface, an influx of warm air brought in by the wind (warm advection), or air moving over a warm surface.
A rising parcel of air that does not exchange heat with its surroundings is an example of
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If rising air cools to its dew-point temperature, the relative humidity becomes ____.
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Cumulus clouds are a common phenomenon over cool water surfaces.
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Rain shadows form on the ____________________ side of mountains.
(Short Answer)
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An afternoon sky full of cumulus humilis clouds with little vertical growth indicates ____ weather.
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Environmental lapse rate and dry adiabatic rate are different expressions for the same phenomenon.
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Vertical mixing of air tends to ____________________ the environmental lapse rate.
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Lenticular clouds form on the ____________________ side of mountains.
(Short Answer)
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When the environmental lapse rate exceeds the dry adiabatic rate, the lapse rate is called ____________________.
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The potential instability brought about by the lifting of a stable layer whose surface is humid and whose top is "dry" is called ____________________.
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Inversions that form as air slowly sinks over a large area are called ____ inversions.
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A layer of altostratus can change into one of altocumulus, if the top of the original cloud deck cools while the bottom warms.
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Suppose you observe lenticular clouds that appear to be motionless. Is the air in the vicinity of the cloud motionless? Explain.
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If the environmental lapse rate is less than the moist adiabatic rate, the atmosphere is
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List four primary ways clouds form, and describe the formation of one cloud type by each method.
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