In a subsidence inversion, what happens to the sinking air?

In a subsidence inversion, as air sinks, it undergoes adiabatic compression, which leads to an increase in temperature. This phenomenon occurs because as the air descends, the pressure increases, and this increase in pressure causes the air to warm. The temperature of the air near the surface ends up being warmer than the air above it, which creates a stable layer of air that can suppress upward movement and cloud formation. This is significant in meteorology because subsidence inversions can contribute to clear skies and stable weather conditions, often leading to dry weather rather than precipitation or thunderstorms.