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The atmosphere is unstable when the environmental lapse rate is

  • A.Negative
  • B.Greater than the dry adiabatic lapse rate
  • C.Less than the dry adiabatic lapse rate
  • D.Exactly equal to it

Answer: B

Correct answer: Greater than the dry adiabatic lapse rate

The atmosphere is unstable when the environmental lapse rate exceeds the dry adiabatic rate of about \( 9.8 \) degrees per kilometre - the superadiabatic condition. A parcel displaced upward cools at the adiabatic rate, but the surrounding air cools faster with height, so the parcel finds itself warmer and less dense than its surroundings and keeps rising.

If the environmental rate is less than adiabatic the parcel becomes colder and denser than its surroundings and sinks back, which is stable. Equality gives neutral conditions, in which a displaced parcel neither rises nor sinks. Instability favours vigorous vertical mixing and rapid dilution of a plume.

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