Which phenomenon results from temperature inversion?

Temperature inversion occurs when a layer of warm air traps cooler air near the surface, which can prevent the normal vertical mixing of the atmosphere. This phenomenon can lead to the formation of fog because the warmer air aloft can reduce the vertical movement of air, allowing the cooler, moist air at the surface to condense when it's cooled further, especially during the night or early morning. The trapped humidity can saturate the air, leading to the development of fog.

While other weather phenomena can occur in general atmospheric conditions, fog is particularly associated with temperature inversions due to these specific interactions between air layers and moisture.