To test the theoretical picture more stringently, we have investigated the adjustment of the turbulence to a forest canopy, using data taken in a wind tunnel study utilising laser-doppler velocimetry. Very detailed spatial sampling was used to resolve both the temporal and spatial adjustment of the mean flow and turbulence adequately (35 lateral positions across the edge spanning a range of -10 to 50 canopy heights, at 22 heights between 0 and 3 canopy heights in the vertical, and at approximately 2kHz). The adjustment of the mean wind vector follows the theoretical/canonical view, with adjustment largely completed within N Lc where Lc is the canopy adjustment length defined as 1/(drag coefficient X leaf area per unit volume). We will illustrate the co-adjustment of the turbulence through an analysis of the response of both of the second order moments and of the power and co-spectra. Specific consideration will be given to whether these data support the canopy-eddy generation picture of turbulence adjustment, the relative scales over which the adjustment processes occur and the presence of novel features in this highly resolved experiment.