CDNC data is derived from MODIS-retrieved cloud optical thickness and
cloud-top droplet effective radius. Liquid water clouds only are used,
and COD and CDR are restricted to their most reliable values (4um <= CDR
<= 30um and 4 <= COD <= 70; Nakajima and King, J. Atmos. Sci., 1990).
However, for MODIS-retrieved CDR, problems are known (Breon and
Doutriaux-Boucher, IEEE Trans. Geosci. Remote Sens., 2005). The
assumption of adiabacity may not necessarily be valid, even though large
regions are considered.
We recommend to use CDNC for statistical studies rather than to rely on
absolute accuracy in single regions or short time-periods