What function does a subsidence inversion typically serve?

A subsidence inversion occurs when a layer of warm air traps cooler air at the surface, which can restrict vertical mixing of the atmosphere. This phenomenon is characterized by descending air, which compresses and warms as it sinks, leading to drier conditions close to the surface. As the air descends, it inhibits cloud formation and maintains a stable atmosphere, thus significantly impacting weather conditions in the area.

This warming and drying effect of the descending air is particularly relevant in the context of wildland fire behavior since it can lead to lower humidity levels and can create conditions that are more conducive to fire ignition and spread. Understanding subsidence inversions allows fire management professionals to anticipate changes in fire behavior that could arise from these atmospheric conditions.