What weather conditions are expected during a low-level temperature inversion with high relative humidity?

During a low-level temperature inversion with high relative humidity, stable air is trapped beneath a layer of warmer air, leading to specific weather conditions. As the air near the ground cools, moisture in the air condenses, often resulting in fog, haze, or low clouds. This phenomenon typically reduces visibility, as the presence of moisture leads to obstructions in the atmosphere caused by these moisture particles.

In addition to fog and haze, the stability of the air during a temperature inversion discourages vertical mixing, which contributes to the smooth air conditions. As the cooler air remains stagnant, it allows for the persistence of the humidity, leading to those low clouds or fog that characterizes the environment during such a weather event.

The other weather conditions mentioned in the incorrect options do not align with what is typical in a temperature inversion scenario. Clear skies with high visibility would not be observed in such circumstances, nor would windy conditions or thunderstorms be common, given that inversions tend to stabilize the atmosphere rather than encourage turbulence or severe weather.