What defines a cold front in terms of precipitation?

A cold front is characterized by the rapid lifting of warm, moist air as it meets colder air, which can lead to significant weather changes. Specifically, precipitation associated with a cold front typically occurs at the leading edge of the front. This is due to the abrupt boundary created when the colder, denser air pushes under the warmer air, forcing the warm air to rise rapidly. As the warm air ascends, it cools and condenses, resulting in cloud formation and precipitation, often in the form of heavy rain, thunderstorms, or snow, depending on the temperature profile.

This aligns with the typical weather patterns observed during cold fronts, where storms can develop preceding the front itself. Therefore, precipitation generated by cold fronts is most commonly found at the front's leading edge, distinguishing it from other frontal types and their associated weather phenomena.