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- Capping_inversion abstract "A capping inversion is an elevated inversion layer that caps a convective boundary layer. The boundary layer is the part of the atmosphere which is closest to the ground. Normally, the sun heats the ground, which in turn heats the air just above it. Thermals form when this warm air rises into the cold air (warm air is less dense than cold air), a process described by convection. A convective layer such as this has the potential for cloud formation, since condensation occurs as the warm air rises and cools.An inversion occurs when the normal temperature (warm air below, cold air above) profile is reversed, creating a stable configuration of dense, cold air sitting below lighter, warm air. An elevated inversion layer is thus a region of warm air above a region of cold air, but higher in the atmosphere (generally not touching the surface).A capping inversion occurs when there is a boundary layer with a normal temperature profile (warm air rising into cooler air) and the layer above that is an inversion layer (cooler air below warm air). Cloud formation from the lower layer is \"capped\" by the inversion layer. If the capping inversion layer or \"cap\" is too strong (too close to the surface), it will prevent thunderstorms from developing. A strong cap can result in foggy conditions. However, if the air at the surface is unstable enough, strong updrafts can be forced through the capping inversion. This selective process of only allowing the strongest updrafts to form thunderstorms often results in outbreaks of severe weather.".
- Capping_inversion thumbnail Kreuzberg_(Rhoen).JPG?width=300.
- Capping_inversion wikiPageExternalLink search?id=capping-inversion1.
- Capping_inversion wikiPageExternalLink Capping_inversion.
- Capping_inversion wikiPageID "224303".
- Capping_inversion wikiPageLength "2515".
- Capping_inversion wikiPageOutDegree "16".
- Capping_inversion wikiPageRevisionID "649329340".
- Capping_inversion wikiPageWikiLink Category:Atmospheric_thermodynamics.
- Capping_inversion wikiPageWikiLink Category:Boundary_layer_meteorology.
- Capping_inversion wikiPageWikiLink Condensation.
- Capping_inversion wikiPageWikiLink Convection.
- Capping_inversion wikiPageWikiLink Convective_available_potential_energy.
- Capping_inversion wikiPageWikiLink Convective_inhibition.
- Capping_inversion wikiPageWikiLink Convective_instability.
- Capping_inversion wikiPageWikiLink Density.
- Capping_inversion wikiPageWikiLink Fog.
- Capping_inversion wikiPageWikiLink Inversion_(meteorology).
- Capping_inversion wikiPageWikiLink Planetary_boundary_layer.
- Capping_inversion wikiPageWikiLink Severe_weather.
- Capping_inversion wikiPageWikiLink Thermal.
- Capping_inversion wikiPageWikiLink Thunderstorm.
- Capping_inversion wikiPageWikiLink File:Atmospheric_boundary_layer.svg.
- Capping_inversion wikiPageWikiLink File:Kreuzberg_(Rhoen).JPG.
- Capping_inversion wikiPageWikiLinkText "Capping inversion".
- Capping_inversion wikiPageWikiLinkText "cap".
- Capping_inversion wikiPageWikiLinkText "capped".
- Capping_inversion wikiPageWikiLinkText "capping inversion".
- Capping_inversion wikiPageWikiLinkText "capping".
- Capping_inversion wikiPageWikiLinkText "inversion layer".
- Capping_inversion wikiPageUsesTemplate Template:Climate-stub.
- Capping_inversion wikiPageUsesTemplate Template:Meteorological_variables.
- Capping_inversion wikiPageUsesTemplate Template:No_footnotes.
- Capping_inversion subject Category:Atmospheric_thermodynamics.
- Capping_inversion subject Category:Boundary_layer_meteorology.
- Capping_inversion hypernym Layer.
- Capping_inversion type AnatomicalStructure.
- Capping_inversion type Layer.
- Capping_inversion type Redirect.
- Capping_inversion type Science.
- Capping_inversion type Thermodynamic.
- Capping_inversion comment "A capping inversion is an elevated inversion layer that caps a convective boundary layer. The boundary layer is the part of the atmosphere which is closest to the ground. Normally, the sun heats the ground, which in turn heats the air just above it. Thermals form when this warm air rises into the cold air (warm air is less dense than cold air), a process described by convection.".
- Capping_inversion label "Capping inversion".
- Capping_inversion sameAs Q5036188.
- Capping_inversion sameAs Inwersja_nakrywająca.
- Capping_inversion sameAs m.01gph0.
- Capping_inversion sameAs Q5036188.
- Capping_inversion wasDerivedFrom Capping_inversion?oldid=649329340.
- Capping_inversion depiction Kreuzberg_(Rhoen).JPG.
- Capping_inversion isPrimaryTopicOf Capping_inversion.