ell as increases the stratiform
     cloud fraction.

     This parameterization was developed by Moorthi and Suarez 
     (see reference), with local modifications by Joe  Sirutis and
     Steve Klein. The local modifications include: 1) re-evaporation
     of convective scale precip was added, 2) the entrainment parameter
     was made a function of cloud type, and was used in tuning the 
     moisture distribution produced by the scheme, 3) an option of 
     detraining condensed liquid and ice into stra