atmosphere_convective_inhibition

Convective inhibition is the amount of energy per unit mass required to overcome the negatively buoyant energy exerted by the environment on a parcel of air. Convective inhibition is often abbreviated as "CIN" or "CINH". It is calculated by integrating the negative temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from a given starting height to its equilibrium level. A coordinate variable of original_air_pressure_of_lifted_parcel should be specified to indicate the starting height of the lifted parcel.
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  • Proposls with this term version:
  • Proposal: Seth McGinnis [new standard names for CIN, LFC,LCL; upd]
  • Proposal: Jonathan Gregory [error in canonical units of atmosphere_c]

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