What type of front is generally associated with low-pressure systems?

A warm front is typically associated with low-pressure systems because it forms when warm, moist air rises over a mass of cooler, denser air. This process leads to cloud formation and precipitation as the warm air cools and condenses at higher altitudes. The gradual slope of a warm front can result in extended periods of light to moderate rain. In low-pressure areas, these fronts often lead to the development of cloud cover and precipitation patterns that are characteristic of stormy weather.

The other types of fronts also interact with low-pressure systems but have different characteristics. Cold fronts are associated with more violent weather changes, often leading to thunderstorms and abrupt temperature drops. Occluded fronts occur when a cold front overtakes a warm front, often leading to complex weather systems but may not be as directly associated with atmospheric lifting as warm fronts. Stationary fronts can bring extended periods of cloudy and wet weather but are characterized by a lack of significant movement, making them less directly linked to the dynamics of low-pressure systems compared to warm fronts.