In
meteorology
Meteorology is a branch of the atmospheric sciences (which include atmospheric chemistry and physics) with a major focus on weather forecasting. The study of meteorology dates back millennia, though significant progress in meteorology did no ...
, the equilibrium level (EL), or level of neutral buoyancy (LNB), or limit of convection (LOC), is the height at which a rising
parcel
Parcel may refer to:
* Parcels (band), an Australian modern soul band
* Parcel (consignment), an individual consignment of cargo for shipment
* ''Parcel'' (film), 2019 Bengali film
* Parcel (package), sent through the mail or package delivery
...
of
air is at the same
temperature
Temperature is a physical quantity that expresses quantitatively the perceptions of hotness and coldness. Temperature is measured with a thermometer.
Thermometers are calibrated in various temperature scales that historically have relied on ...
as its environment.

This means that unstable air is now stable when it reaches the equilibrium level and
convection
Convection is single or multiphase fluid flow that occurs spontaneously due to the combined effects of material property heterogeneity and body forces on a fluid, most commonly density and gravity (see buoyancy). When the cause of the c ...
stops. This level is often near the
tropopause and can be indicated as near where the
anvil of a
thunderstorm because it is where the thunderstorm
updraft is finally cut off, except in the case of
overshooting tops where it continues rising to the
maximum parcel level (MPL) due to momentum. More precisely, the cumulonimbus will stop rising around a few kilometres prior to reaching the level of neutral buoyancy and on average anvil glaciation occurs at a higher altitude over land than over sea (despite little difference in LNB from land to sea).
See also
*
Atmospheric thermodynamics
*
Convective instability
*
Level of free convection
*
Lifted condensation level
References
External links
The Difference Between the Equilibrium Level and Maximum Parcel Level
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Severe weather and convection
Atmospheric thermodynamics
Buoyancy