Concept information
Preferred term
atmosphere_level_of_free_convection_wrt_surface
Definition
- The level of free convection is the altitude where the temperature of the environment decreases faster than the moist adiabatic lapse rate of a saturated air parcel at the same level. It is calculated by lifting a parcel of air dry adiabatically from the surface to the LCL (lifting condensation level), then moist adiabatically until the parcel temperature is equal to the ambient temperature.
Note
- Mapping to be determined
URI
https://vocab.met.no/CFSTDN/atmosphere_level_of_free_convection_wrt_surface
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