Atmospheric stability is judged by comparing the ambient temperature gradient to the dry adiabatic rate that a rising parcel would follow. If the ambient rate is smaller than this reference, a displaced parcel cools faster than its surroundings and sinks back, giving a stable, sub-adiabatic atmosphere. If the ambient rate exactly matches the reference, the atmosphere is considered neutral. The scenario in the question is the opposite extreme, where the ambient rate is larger than the reference rate, meaning a rising parcel stays buoyant and continues rising even more strongly than under ordinary adiabatic behaviour; this exaggerated instability is specifically named the super-adiabatic condition.
Therefore, the correct answer is Super adiabatic lapse rate.
Thinking in terms of atmospheric stability categories rather than definitions alone helps settle this quickly.
Placing the described scenario, ambient rate greater than adiabatic rate, into the standard stability classification points directly to the unstable, super-adiabatic case.
Therefore, the correct answer is Super adiabatic lapse rate.