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- Q6795904 subject Q7609667.
- Q6795904 subject Q8275066.
- Q6795904 abstract "The maximum parcel level (MPL) is the highest level in the atmosphere that a moist convectively rising air parcel will reach after ascending from the level of free convection (LFC) through the free convective layer (FCL) and reaching the equilibrium level (EL), near the tropopause. As the parcel rises through the FCL it expands adiabatically causing its temperature to drop, often below the temperature of its surroundings, and eventually lose buoyancy. Because of this, the EL is approximately the region where the distinct flat tops (called anvils) often observed on cumulonimbus clouds form. If the air parcel ascended quickly enough then it retains momentum after it has cooled and continues rising past the EL, ceasing at the MPL (visually represented by the overshooting top, above the anvil).".
- Q6795904 wikiPageExternalLink ?request=get-abstract&doi=10.1175%2F1520-0469(1998)055%3C3440%3AEADINS%3E2.0.CO%3B2.
- Q6795904 wikiPageExternalLink ?request=get-abstract&issn=1520-0469&volume=055&issue=23&page=3417.
- Q6795904 wikiPageExternalLink 165.
- Q6795904 wikiPageExternalLink 311.
- Q6795904 wikiPageWikiLink Q104363.
- Q6795904 wikiPageWikiLink Q1358304.
- Q6795904 wikiPageWikiLink Q160329.
- Q6795904 wikiPageWikiLink Q182311.
- Q6795904 wikiPageWikiLink Q186433.
- Q6795904 wikiPageWikiLink Q2990712.
- Q6795904 wikiPageWikiLink Q3173757.
- Q6795904 wikiPageWikiLink Q3186958.
- Q6795904 wikiPageWikiLink Q3230.
- Q6795904 wikiPageWikiLink Q3271065.
- Q6795904 wikiPageWikiLink Q41273.
- Q6795904 wikiPageWikiLink Q4356508.
- Q6795904 wikiPageWikiLink Q5500209.
- Q6795904 wikiPageWikiLink Q584909.
- Q6795904 wikiPageWikiLink Q600596.
- Q6795904 wikiPageWikiLink Q6497624.
- Q6795904 wikiPageWikiLink Q7609667.
- Q6795904 wikiPageWikiLink Q8275066.
- Q6795904 wikiPageWikiLink Q931652.
- Q6795904 comment "The maximum parcel level (MPL) is the highest level in the atmosphere that a moist convectively rising air parcel will reach after ascending from the level of free convection (LFC) through the free convective layer (FCL) and reaching the equilibrium level (EL), near the tropopause. As the parcel rises through the FCL it expands adiabatically causing its temperature to drop, often below the temperature of its surroundings, and eventually lose buoyancy.".
- Q6795904 label "Maximum parcel level".