What weather condition is commonly associated with low-level inversions?

Low-level inversions are atmospheric conditions where a layer of warm air traps cooler air at the surface, leading to stagnant air. This phenomenon often occurs during the night or early morning, especially in valleys or areas with clear skies. As the cooler air is trapped, moisture in this air can condense, leading to the formation of fog and haze. This effect is quite common in locations where there are stable weather conditions with little wind, allowing for moisture to remain close to the ground and form these cloudy or hazy conditions.

While other weather conditions, such as clear blue skies or high temperatures may influence the possibility of inversions forming, they are not directly associated with the resulting phenomena that inversions often cause, such as fog and haze. Similarly, dry conditions do not typically coincide with low-level inversions, as inversions tend to retain moisture rather than lead to dryness.