What is typically associated with a warm front?

A warm front is a boundary that forms when a warm air mass moves in to replace a cooler air mass. As this warm air rises over the cooler air, it cools and condenses, leading to the formation of clouds and precipitation. This process typically results in gradual changes in weather conditions, which may include light to moderate rain, a steady drizzle, or overcast skies.

Thus, precipitation is directly associated with a warm front as the primary meteorological phenomenon that occurs when warm air rises and cools, resulting in the release of moisture. This is in contrast to other weather phenomena, which may not occur specifically with a warm front.