Equilibrium Level
Term · Meteorology and atmospheric science · MLC-T-MET-000881
(EL) - On a sounding, the level above the level of free convection (LFC) at which the temperature of a rising air parcel again equals the temperature of the environment. The height of the EL is the height at which thunderstorm updrafts no longer accelerate upward. Thus, to a close approximation, it represents the height of expected (or ongoing) thunderstorm tops.
| Identifier | MLC-T-MET-000881 |
|---|---|
| Field | Meteorology and atmospheric science |
| References | NWS Glossary |
Record as JSON
{
"id": "MLC-T-MET-000881",
"term": "Equilibrium Level",
"field": "Meteorology and atmospheric science",
"definition": "(EL) - On a sounding, the level above the level of free convection (LFC) at which the temperature of a rising air parcel again equals the temperature of the environment. The height of the EL is the height at which thunderstorm updrafts no longer accelerate upward. Thus, to a close approximation, it represents the height of expected (or ongoing) thunderstorm tops.",
"references": [
"NWS Glossary"
],
"url": "https://mlchart.com/terminology/meteorology/equilibrium-level/"
}
Record 881 of 3,164 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.