Environmental lapse rate and dry adiabatic rate are different expressions for the same phenomenon.
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Q7: If an air parcel is given a
Q8: The temperature of rising air at a
Q9: The combination of warming the surface and
Q10: Subsidence inversions are just as common on
Q11: Cumulus clouds are a common phenomenon over
Q13: Convective instability associated with severe thunderstorms and
Q14: It is possible for a layer of
Q15: Subsidence has no effect on atmospheric stability.
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Q17: Sinking air sometimes cools adiabatically.
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