Estimation of lifted condensation level (LCL)
Since Parmesan is fit for general meteorological calculations we can add a function that finds the lifted condensation level (commonly named LCL). You can read more about it here.
TL:DR version definition: LCL is the height from the ground where an air parcel would saturate if lifted adiabatically. This is a very direct way to get the height of the cumulus-cloud base / cover (i.e. to know at which altitude clouds are formed).
In general, low / high cloud formations can affect a lot of procedures that we are investigating, like fluxes, vertical profiles etc... It could be valuable for @nobodyinperson and his project too, and it only requires values of temperature and relative humidity (or dew point temperature, stuff we already measure).
A very good and easy to read article about this topic can be found here. A formula as simple as Eq. (22) from that link can be used and there is also the explanation around it. Then, there is a deeper analysis for it in this paper, if anyone is interested.