The point where saturation begins in a rising air parcel is

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The lifting condensation level (LCL) is the altitude at which a rising air parcel reaches saturation and starts to cool at the moist adiabatic rate. At this point, the air parcel's temperature will decrease at a slower rate due to the release of latent heat of condensation as water vapor condenses into liquid droplets. Cloud formation typically occurs at or near the lifting condensation level. Therefore, the point where saturation begins in a rising air parcel is the lifting condensation level.

The Point Where Saturation Begins in a Rising Air Parcel