In the context of cloud structure, what role does a temperature inversion play?

A temperature inversion occurs when a layer of warm air traps cooler air near the surface, which can significantly influence cloud structure and weather patterns. This phenomenon plays a crucial role in trapping moisture within the cooler air layer, leading to the formation of stratified cloud types, such as stratus clouds. The stable, warm air above prevents the cooler air below from rising, inhibiting vertical development of clouds that typically results in more dynamic weather conditions.

In this scenario, moisture that evaporates from the surface is not able to rise and disperse as it normally would due to the inversion. Instead, it accumulates in the cooler air, contributing to cloud formation and creating a layer of clouds that can lead to overcast conditions. This stratification is often associated with prolonged periods of cloudy weather and can impact visibility and precipitation patterns in the area. Understanding how temperature inversions create this cloud stratification is key in predicting weather and assessing conditions for activities such as sailing.