Convective available potential energy
Builds on Lapse rate
Definition
Consider a hydrostatic atmosphere with gravitational acceleration . Lift an air parcel from near the surface, dry adiabatically up to saturation and then moist adiabatically. Let be the virtual temperature of the parcel and that of the environment at height . The level of free convection is the lowest height above which the parcel is warmer than the environment, . The equilibrium level is the height above at which the parcel first becomes as cold as the environment again. The convective available potential energy is If there is no level of free convection, .
Remarks
The integrand is the buoyancy acceleration of the parcel, so CAPE has units of J/kg. With the hydrostatic relation and the ideal gas law, CAPE , where is the gas constant of dry air and , are the pressures at and . The negative buoyancy below gives the convective inhibition.
Example: if K and K on the whole layer from km to km, then CAPE J/kg. Parcel theory then bounds the updraught speed by m/s.
Non-example: suppose the environmental lapse rate is smaller than the moist adiabatic lapse rate at every level. Then a lifted parcel stays colder than its surroundings, there is no level of free convection, and CAPE is zero.
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- Lapse rate concept
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About this page
| Tag | 13ZJFCMHCE |
|---|---|
| URI | m2://13ZJFCMHCE |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A10 |
| Defines | Convective available potential energy |
| Uses | Lapse rate |
| Changed | 3 November 2026 |
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