The phrase "an inversion layer" is correct and usable in written English.
It is typically used in scientific contexts, particularly in meteorology, to describe a layer of the atmosphere where temperature increases with altitude, which can trap pollutants.
Example: "The presence of an inversion layer can lead to poor air quality in urban areas, as it prevents the dispersion of pollutants."
Alternatives: "temperature inversion" or "inversion zone".
"As long as you don't have an inversion layer," the Dodgers broadcaster Rick Monday said.
From this angle, structural features in the atmosphere, like an inversion layer, could mask the presence of water.
Strictly speaking, it is simply a medium in which clouds can form a layer of air trapped between the surface of the cold ocean and an inversion layer above formed by hot air spilling out of the high desert.
During parties at our house, a cloud like an inversion layer would fill the downstairs, and the next morning, when Anne and I went down to pour bowls of cereal for ourselves and wait for cartoons to come on, there would be overflowing ashtrays everywhere, and sodden cigarette butts floating in the bottoms of almost-empty beer glasses, whose sides were spider-webbed with dried foam.
This indicates that an inversion layer at the MoS2/n-GaAs interface is formed [18].
Even though the frequency is small, this fact suggests that we should carefully investigate the atmospheric profile, especially the existence of an inversion layer.
A strong inversion layer confined the smoke to a 2,000-foot-thick 2,000-foot-thick 2,000-foot-thickSan Bernardino and Riverside Counties.
It is demonstrated that these features are related to the existence of a strong inversion layer of holes at the c-Si surface of (p) a-Si H/(n) c-Si structures, a-Si H/a strong inversion layer of electrons at the c-Si surfand of (n) a-Si:H/(p) c-Si hetorojunctions.
In one, the plate is composed of a layer of 36° rotated y-cut LiNbO3 with a ferroelectric inversion layer.
A temperature inversion layer frequently appeared below 300 m altitude at night, causing an overestimation of T m by 2 to 4 K, which, in turn, introduced an error in PWV of about 0.5 mm.
Solar heating of the particle layers creates a temperature inversion layer in Titan's stratosphere, preventing the smog layer from dissipating by convection.
