Here, a nested LES of turbulent flow within and above a forest canopy on an isolated two-dimensional hill is analyzed in details and validated against wind-tunnel data. The model is shown to reproduce accurately the main features observed over a forested hill. The simulations also confirm recent observations on the intermittent character of the recirculation region behind the hill and on the dominance of sweep motions in momentum transfer at canopy top all along the hill.
The main characteristics of turbulent structures are also investigated from vorticity fields and two-point velocity correlations simulated across the hill. It is shown that the streamwise wind velocity upwind from the ridge is not correlated with the flow within the wake region but only with the flow above it, while in the wake region, the streamwise wind velocity at canopy top is only correlated with the flow within the wake region. This result may suggest that turbulence within the wake region results from the superimposition of various turbulent structures: i) large structures induced by the elevated shear layer that may result from Kelvin-Helmoltz instabilities, ii) structures induced by the adverse pressure gradient at the lee-side foot of the hill, and iii) structures induced by the presence of the canopy itself. Implications of hilly terrain on canopy-atmosphere exchanges and tree vulnerability to windload are also briefly discussed.