Compare this to the Lifting Condensation Level ( LCL ) where the air is lifted and cooled without first increasing the surface temperature.
2.
This altitude is known as the lifting condensation level ( LCL ) when mechanical lift is present and the convective condensation level ( CCL ) when mechanical lift is absent, in which case, the parcel must be heated from below to its convective temperature.
3.
If the environmental lapse rate is larger than the dry adiabatic lapse rate, it has a superadiabatic lapse rate, the air is absolutely unstable a parcel of air will gain buoyancy as it rises both below and above the lifting condensation level or convective condensation level.
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