Which characteristic is commonly associated with a temperature inversion?

A temperature inversion is a situation in the atmosphere where the typical temperature gradient is reversed, meaning that air temperature increases with altitude rather than decreases. This phenomenon creates a stable layer of air, as the warmer air above hinders vertical mixing and the rise of cooler air below.

In stable conditions characterized by a temperature inversion, there is often a layer of cooler air trapped beneath the warmer air. This stability prevents the cooler air from rising, leading to a more homogenized and less turbulent atmosphere. As a result, weather phenomena associated with stability, such as fog, haze, or low cloud cover, can occur.

The other characteristics listed do not align with the properties of a temperature inversion. Changes in wind speed, for instance, or the presence of a rapidly changing air mass, suggest dynamic and unstable conditions rather than the stability brought about by temperature inversions.