a layer of warm air is formed on top of a layer of cold air

Temperature inversion is a phenomenon where a layer of warm air is formed on top of a layer of cold air, unlike in normal atmospheric conditions.

An increase of temperature with height

An increase of temperature with height is known as a temperature inversion.

a thin layer of the atmosphere

A temperature inversion is a thin layer of the atmosphere where the normal decrease in temperature with height switches to the temperature increasing with height.

a reversal of the normal distribution of temperature near the ground, in which a layer of colder air is overlain by a layer of warmer air

Temperature inversion is a reversal of the normal distribution of temperature near the ground, in which a layer of colder air is overlain by a layer of warmer air.

a weather condition called a temperature inversion

In London, Tokyo, New York and other cites, a weather condition called a temperature inversion allows smog to hang over the city for several days at a time.

a layer in the atmosphere in which air temperature increases with height

According to the National Weather Service, “a temperature inversion is a layer in the atmosphere in which air temperature increases with height.”

by increasing temperature with altitude

Temperature inversions are characterized by increasing temperature with altitude and are common on nights with limited cloud cover and light to no wind.

a weather condition that can allow pesticides to move beyond the field of application

A temperature inversion is a weather condition that can allow pesticides to move beyond the field of application.

a layer of reversal of the normal decrease in temperature with an increase in altitude

A temperature inversion is a layer of reversal of the normal decrease in temperature with an increase in altitude.

a deviation from the normal meteorological phenomenon

Well, this is often caused by a Temperature Inversion, and a Temperature Inversion’s a deviation from the normal meteorological phenomenon.

increase of temperature with altitude

Generally the temperature inversion means increase of temperature with altitude .

This reversal of the usual fall of temperature with height above the ground

This reversal of the usual fall of temperature with height above the ground is called a 'temperature inversion' and it acts as a sort of atmospheric lid, trapping pollution, cloud, and mist in the cool layer of air near the ground.

layers

Temperature inversions are usually layers rather than sharp lines separating regions of different temperature.

a weather phenomenon in which the air at the earth’s surface is cooler than the air above the air – a situation different than the norm

Temperature inversion is a weather phenomenon in which the air at the earth’s surface is cooler than the air above the air – a situation different than the norm, said Christopher “Chip” Redmond, manager of Kansas Mesonet.

an area above the surface

Temperature generally tends to decrease with height, but a temperature inversion is an area above the surface (at some point) where the temperature in our vertical atmosphere actually increases (or may stay the same).

a result of other weather conditions in an area

Temperature inversions are a result of other weather conditions in an area.

The increase in temperature above the tropopause

The increase in temperature above the tropopause (upper part of the figure) is known as an inversion, because temperature normally decreases with height.

another weather phenomenon linked to atmospheric odors, but rather

Temperature inversions are another weather phenomenon linked to atmospheric odors, but rather than trigger a certain smell, they exacerbate odors that are already airborne.

cloud inversion

A cloud inversion, also known as a 'temperature inversion', occurs when the air near the ground is cooler than the air above the air .

a condition in which a layer of warm air prevents cooler rising air from escaping into higher parts of the atmosphere

a temperature inversion is a condition in which a layer of warm air prevents cooler rising air from escaping into higher parts of the atmosphere.