The in uence of a forest canopy on top - down and bottom - up diffusion in the planetary boundary layer

Results from two nested-grid large-eddy simulations comparing cases with and without a plant canopy are presented. Through comparisons of numerically generated mean and turbulence statistics, the in uence of a plant canopy with a leaf area index of two is shown to modify the air  ow compared with an identical case without plants. Investigations of instantaneous Ž elds and spatial spectra show that a plant canopy alters the spatial structure of turbulence and acts to shift the dominant scale to a scale on the order of the canopy height. Distributed drag and scalar sources, representing the presence of a scalar emitting deciduous forest, have little in uence on top-down diffusion, but enhanced mixing and increased turbulence intensities result in a dramatic modiŽ cation to bottom-up scalar diffusion up to»4.5 times the height of the canopy. Use of previously proposed bottom-up gradient function with observations of scalar gradients under unstable stability conditions at 50 m over a 25 m tall forest (leaf area index of two) are shown to lead to an underestimate of the scalar emission  ux by a factor of four. New top-down and bottom-up functions are proposed to include these canopy-induced effects for this particular canopy.