What defines the term 'Super Saturation' in cloud terminology?

The term 'Super Saturation' in cloud terminology refers to conditions where relative humidity exceeds 100%. This is a critical concept in meteorology, as it indicates that the air contains more moisture than it can hold at a given temperature, leading to potential condensation. Under super saturated conditions, the moisture present can begin to condense out into droplets, forming clouds or precipitation, even though the relative humidity has surpassed the saturation point.

In practical terms, when the air is super saturated, it becomes unstable, and the excess moisture can lead to cloud formation and various phenomena such as fog or precipitation. This is significant in understanding weather patterns and predicting the behavior of clouds in different atmospheric conditions.