final_air_pressure_of_lifted_parcel
Various stability and convective potential indices are calculated by "lifting" a parcel of air: moving it dry adiabatically from a starting height (often the surface) to the Lifting Condensation Level, and then wet adiabatically from there to an ending height (often the top of the data/model/atmosphere). original_air_pressure_of_lifted_parcel and final_air_pressure_of_lifted_parcel are the pressure heights at the start and end of lifting, respectively.
List containing this term version:
CF (27)
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Proposls with this term version:
Proposal: Jonathan Wrotny & Seth McGinnis [new standard name: lifted_index; atmosph]
Proposal: Alison Pamment [Standard names for CF trac ticket #143]
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