Session Objectives
Session 6: Atmospheric Stability
Upon completion of this session, a participant should be able to
do the following:
- List and describe four major mechanisms which lift air,
causing expansion and cooling.
- Describe the differences between the dry adiabatic, moist
adiabatic, and pseudoadiabatic lapse rates.
- Explain why moist air is more buoyant than dry air at the
same temperature and pressure.
- For a dry atmosphere, compare the lapse rate of a rising air
parcel to the lapse rate of the environment in a stable, neutral,
and unstable atmosphere. Explain how the difference in the lapse
rate of the parcel and the environment affect the vertical
movement of the parcel in the atmosphere.
- Explain how the presence of water vapor affects the lapse
rate of a rising air parcel once the parcel becomes saturated.
- Explain how the unequal distribution of water vapor in an
initially stable layer of air can influence the stability of the
layer if the layer is lifted.
- Describe the effect of entrainment of air into a rising
parcel has on the stability of the atmosphere.
- Describe how various conditions of stability of the
atmosphere relate to the dispersion of pollutants.
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The
Shodor
Education Foundation, Inc.
Copyright © 1996