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- Q4356508 subject Q15292066.
- Q4356508 subject Q7609667.
- Q4356508 subject Q8275066.
- Q4356508 abstract "In meteorology, the equilibrium level (EL), or level of neutral buoyancy (LNB), or limit of convection (LOC), is the height at which a rising parcel of air is at the same temperature as its environment. This means that unstable air is now stable when it reaches the equilibrium level and convection 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).".
- Q4356508 thumbnail Meteorology_thermodynamic_en.svg?width=300.
- Q4356508 wikiPageExternalLink identity-2.htm.
- Q4356508 wikiPageExternalLink 165.
- Q4356508 wikiPageWikiLink Q11466.
- Q4356508 wikiPageWikiLink Q15292066.
- Q4356508 wikiPageWikiLink Q182311.
- Q4356508 wikiPageWikiLink Q186433.
- Q4356508 wikiPageWikiLink Q25261.
- Q4356508 wikiPageWikiLink Q2857578.
- Q4356508 wikiPageWikiLink Q3055189.
- Q4356508 wikiPageWikiLink Q3173757.
- Q4356508 wikiPageWikiLink Q3230.
- Q4356508 wikiPageWikiLink Q3268911.
- Q4356508 wikiPageWikiLink Q3271065.
- Q4356508 wikiPageWikiLink Q584909.
- Q4356508 wikiPageWikiLink Q600596.
- Q4356508 wikiPageWikiLink Q6795904.
- Q4356508 wikiPageWikiLink Q760129.
- Q4356508 wikiPageWikiLink Q7609667.
- Q4356508 wikiPageWikiLink Q8275066.
- Q4356508 wikiPageWikiLink Q931652.
- Q4356508 comment "In meteorology, the equilibrium level (EL), or level of neutral buoyancy (LNB), or limit of convection (LOC), is the height at which a rising parcel of air is at the same temperature as its environment. This means that unstable air is now stable when it reaches the equilibrium level and convection stops.".
- Q4356508 label "Equilibrium level".
- Q4356508 depiction Meteorology_thermodynamic_en.svg.