level of free convection

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level of free convection [′lev·əl əv ‚frē kən′vek·shən]

(meteorology)

The level at which a parcel of air lifted dry and adiabatically until saturated, and lifted saturated and adiabatically thereafter, would first become warmer than its surroundings in a conditionally unstable atmosphere. Abbreviated LFC.

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