What is a consequence of a temperature inversion on atmospheric stability?

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Multiple Choice

What is a consequence of a temperature inversion on atmospheric stability?

Explanation:
A temperature inversion creates a layer where air gets warmer with height, reversing the usual cooling with altitude. This forms a stable stratification, so a parcel that’s lifted will find itself cooler than its surroundings and tend to sink back. That restoring tendency suppresses vertical motion and convection, making the atmosphere more stable. So the consequence is increased stability. Inversions can also trap pollutants near the surface, but the key point for stability is the strong resistance to vertical mixing.

A temperature inversion creates a layer where air gets warmer with height, reversing the usual cooling with altitude. This forms a stable stratification, so a parcel that’s lifted will find itself cooler than its surroundings and tend to sink back. That restoring tendency suppresses vertical motion and convection, making the atmosphere more stable. So the consequence is increased stability. Inversions can also trap pollutants near the surface, but the key point for stability is the strong resistance to vertical mixing.

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