“…Over the past several years, much attention has been paid to the modulating effects of certain land surface characteristics on the thermodynamic profile within the convective boundary layer (CBL). In particular, surface vegetation and soil moisture have been examined with respect to their ability to partition incoming solar radiation, or insolation, into sensible and latent heating, “H” and “LE,” respectively [ Segal et al , 1988; LeMone et al , 2003; Diak et al , 2004; Holder et al , 2006]. The influence this effect has upon the preferential location of shallow and deep convection has also been studied in great detail [ Rabin et al , 1990; Mahrt et al , 1994; Hong et al , 1995; Segal et al , 1995; Crook , 1996; Rabin and Martin , 1996; Pielke , 2001; Dissing and Verbyla , 2003; Ek and Holtslag , 2004; Kustas et al , 2005; Holt et al , 2006; Childs et al , 2006].…”