A large-eddy simulation(LES) of a cumulus-topped boundary layer (CTBL)
has been made, based on observations gathered on 10 September 1974 du
ring the GARP (Global Atmospheric Research Program) Atlantic Tropical
Experiment (GATE). On this day there were light winds, making buoyancy
production the only important mechanism for generating turbulent kine
tic energy. Cumulus clouds with a depth of a few hundred meters covere
d about 10% of the sky. A comparison between LES results and observed
variances and fluxes will be made. In order to understand the dynamics
of the cumulus, we will investigate the physical mechanisms by which
variances and fluxes are produced in CTBL's. This will be done by anal
yzing the budget equations which describe the time evolution of the va
riances and fluxes. The production, transport and destruction terms, t
hat appear in these equations, will be calculated explicitly with the
LES model. Budgets are calculated from the GATE simulation and two sli
ghtly modified GATE simulations, in which only the initial water vapor
specific humidity is increased. As a result in these two modified GAT
E simulations the vertical extent of the clouds and the cloud cover is
larger. In this way, the influence of the cumulus clouds on the budge
ts can be investigated more thoroughly. Finally, the budgets are compa
red with the results obtained from an earlier simulation based on the
Puerto Rico Field Experiment and other results found in the literature
.