The convective boundary layer (CBL) over domains with meso-gamma-scale (2-2
0 km) heterogeneity is characterized by preferentially located, organized r
olls of characteristic size equivalent to the length-scale of the heterogen
eity. Additionally, random turbulent thermals also develop when the length-
scale of the heterogeneity exceeds 5-10 km. This is due to a complex intera
ction between the horizontal pressure gradient generated by the heterogenei
ty and the buoyancy forcing. Consequently, the corresponding wavelet spectr
um exhibits two peaks - one representing the turbulent thermals at a charac
teristic scale of about 1.5 times the CBL height and another denoting the o
rganized eddies at a scale similar: to that of the heterogeneity. This impl
ies that subgrid-scale parameterizations in models with grid size larger th
an 5-10 km, which account only for random turbulence, are inadequate for he
terogeneous domains. Also, this study may provide a more objective classifi
cation of scales of atmospheric processes.