When a parcel of air is heated over a surface, it expands, thereby lowering its density relative to its surroundings, and experiences a buoyancy force, causing it to rise. Suppose that the ambient air is cold at the bottom and warmer at the top, giving rise to a "thermal inversion." What do you expect would happen to the heated parcel of air if this inversion were sufficiently strong, assuming the parcel expands adiabatically?

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The Answer of When a parcel of air is heated over a surface, it expands, thereby lowering its density relative to its surroundings, and experiences a buoyancy force, causing it to rise. Suppose that the ambient air is cold at the bottom and warmer at the top, giving rise to a "thermal inversion." What do you expect would happen to the heated parcel of air if this inversion were sufficiently strong, assuming the parcel expands adiabatically?

When a Parcel of Air Is Heated Over a Surface