Free convective layer
In atmospheric sciences, the free convective layer is the layer of conditional or potential instability in the troposphere. It is a layer in which rising air can experience positive buoyancy so that deep, moist convection can occur. On an atmospheric sounding, it is the layer between the level of free convection and the equilibrium level. The FCL is important to a variety of convective processes and to severe thunderstorm forecasting.
It is the layer of instability, the "positive area" on thermodynamic diagrams where an ascending air parcel is warmer than its environment. Integrating buoyant energy from the LFC to the EL gives the amount of convective available potential energy, an estimate of the maximum energy available to convection. The depth of the FCL is expressed by the formula:
or
Deep, moist convection is essentially a thunderstorm or thundercloud, although some such convection does not produce lightning and thus not thunder. It is cumulus congestus clouds or cumulonimbus clouds. An air parcel ascending from the near surface layer or boundary layer ) must work through the stable layer of convective inhibition when present. This work comes from sufficiently increasing instability in the low levels by raising the temperature or dew point, or by mechanical lift. Without the aid of mechanical forcing, a parcel must reach its convective temperature before moist convection begins near the convective condensation level (CCL
