The latter data were used to
specify the relative wetness of the surface in each month/season.
AERMET requires both surface meteorological data to drive its
surface energy balance module and morning upper-air data for
its daytime mixing height calculation in which mixing height
increases due to sensible heat transferred from the surface to the
atmospheric boundary layer. The configuration and implementation
of AERSURFACE and AERMET here follow those in
Chusai et al. (2012) mostly, with some adjustment to suit our
Chon Buri application