If the parcel is saturated it is unstable and will rise to the LCL or CCL, and either be halted due to an inversion layer of convective inhibition, or if lifting continues, deep, moist convection ( DMC ) may ensue, as a parcel rises to the level of free convection ( LFC ), after which it enters the free convective layer ( FCL ) and usually rises to the equilibrium level ( EL ).
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Where z _ \ mathrm { f } is the height of the level of free convection and z _ \ mathrm { n } is the height of the equilibrium level ( neutral buoyancy ), where T _ \ mathrm { v, parcel } is the virtual temperature of the specific parcel, where T _ \ mathrm { v, env } is the virtual temperature of the environment, and where g is the sounding diagram ( e . g ., a Skew-T log-P diagram ) using air temperature and dew point data usually measured by a weather balloon.
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