How Is Saturation Achieved To Form Most Clouds - The list below describes the three ways air parcels can become saturated. Adding moisture (or mixing with cool. If a lenticular cloud forms directly over a mountain, it is sometimes called a cap cloud. It should be noted that condensation by itself. If the rate of evaporation is greater than the rate of condensation, a state of undersaturation is reached and no clouds form. Clouds are saturated portions of the atmosphere where small water droplets or ice crystals have fall velocities so slow that they appear visibly. When saturation occurs, moisture becomes visible water droplets in the form of fog and clouds. A cap cloud can form when air that is statically. Clouds will not form unless the air becomes supersaturated, meaning that its relative humidity is slightly greater than 100%.
If a lenticular cloud forms directly over a mountain, it is sometimes called a cap cloud. A cap cloud can form when air that is statically. It should be noted that condensation by itself. Clouds are saturated portions of the atmosphere where small water droplets or ice crystals have fall velocities so slow that they appear visibly. If the rate of evaporation is greater than the rate of condensation, a state of undersaturation is reached and no clouds form. The list below describes the three ways air parcels can become saturated. When saturation occurs, moisture becomes visible water droplets in the form of fog and clouds. Adding moisture (or mixing with cool. Clouds will not form unless the air becomes supersaturated, meaning that its relative humidity is slightly greater than 100%.