What type of front is characterized by gradual temperature transition and steady precipitation?

The type of front characterized by a gradual temperature transition and steady precipitation is indeed the warm front. Warm fronts occur when a warm air mass moves in and gradually rises over a cooler air mass. This lifting of warm air creates an extensive area of cloud cover and leads to prolonged and steady precipitation.

As the warm air ascends, it cools and condenses, forming clouds that tend to cover a large area. This results in a gentle slope where the temperature changes slowly rather than abruptly, which is why the transition is gradual. The precipitation associated with warm fronts is typically steady and can last for several hours or even days, as opposed to the more intense but shorter bursts of rain that often accompany cold fronts.

In contrast, cold fronts generally bring more abrupt temperature changes and are associated with more intense, but shorter-lived, precipitation events. Occluded fronts occur in more complex weather systems and can produce varied weather patterns, while stationary fronts typically lead to prolonged periods of precipitation without significant shifts in temperature.