How does adiabatic cooling impact cloud formation?

Adiabatic cooling occurs when air rises and expands in the atmosphere, leading to a decrease in temperature without heat exchange with the environment. As the air cools, its capacity to hold moisture decreases, causing water vapor to condense into tiny droplets, forming clouds. This process is crucial for cloud formation, as it allows for the accumulation of moisture, which can eventually lead to precipitation. Overall, adiabatic cooling is a key mechanism in the development of clouds and weather systems.