Capping inversion

Capping inversion


A capping inversion is an elevated inversion layer that caps a convective planetary boundary layer, thus inhibiting significant convection.

A capping inversion seen at Polipoli, Maui, Hawaii. November 01, 2012. Source: Wikicommons

The 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 relatively colder air (warm air is less dense than cold air), a process described as convection. Then, this active boundary layer can be called the convective planetary boundary layer. A convective layer such as this has the potential for cloud formation because condensation occurs as the warm air rises and cools. For further information see the separate article on the planetary boundary layer.

Temperature inversion

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 a region of warm air above a region of cold air, but higher in the atmosphere (typically several thousand feet above the surface). There are two primary causes of an elevated inversion layer. Sinking air aloft (subsidence) will warm as it is compressed at higher pressure. Warm advection aloft, warmer air moving over a region, can also produce an elevated inversion layer.

A capping inversion occurs when there is a planetary boundary layer with a normal temperature profile (temperatures decreasing with height) and a layer above that is an inversion layer (temperature increasing with height). Rising parcels of air will now become cooler than the surrounding air and no longer buoyant. Cloud formation from the lower layer is "capped" by the inversion layer. If the capping inversion layer or "cap" is too strong, it will prevent thunderstorms from developing. A strong cap can result in foggy conditions. Although initially a stable situation, a capping inversion can allow the buildup of heat and moisture at low levels, potential fuel for thunderstorms later.

A capping inversion limits the vertical development of clouds. In this image taken near Kreuzberg (Rhön), the inversion is below the top of the mountain tops. Source: Wikicommons

If the capping inversion is weakened or destroyed by solar heating during the day or a change in weather patterns, then convection, often strong, can develop.

Aerial photograph, in the middle of which is the lignite-fired Niederaußem power plant, Wesptpahlia, Germany; its plume clouds (pyrocumulus) break through the visible inversion layer. Source: Wikicommons

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