Exam 6: Stability and Cloud Development

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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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​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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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.

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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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What is meant by the term neutral atmospheric stability?​

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Lenticular clouds form on the ____________________ side of mountains.​

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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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​Sinking air sometimes cools adiabatically.

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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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