What natural phenomenon can occur alongside warm fronts?

A warm front is characterized by the transition zone where warmer air replaces cooler air. This phenomenon typically brings a gradual increase in temperature as the warm air moves in. As the warm air rises over the cooler air, it cools adiabatically and leads to cloud formation, often resulting in layered clouds.

While cloudy skies and precipitation are commonly associated with warm fronts, the gradual temperature increase occurs while the warm front approaches and passes. This change is a significant aspect of warm front weather patterns and is crucial for pilots to understand since it affects flying conditions. Factors such as visibility can also be influenced, but the primary and most straightforward effect of a warm front is the steady rise in temperature.