High-resolution measurements of the three components of the mean and turbulent velocity statistics were previously obtained around a 2-D array of model buildings in the USEPA meteorological wind tunnel. The current results extend the earlier study to include detailed flow measurements around a 3-D array. Seventy-seven cubical buildings (H=0.15m) were placed in the simulated atmospheric boundary layer of the wind tunnel and arranged in an array 11 wide and 7 deep, separated by one building height. A pulsed-wire anemometer was used to measure mean velocity and turbulence statistics. Measurements extended from 3.3H upstream of the building array to 7.5H downstream.
The flow structure around the 3-D building array was found to be very similar to that measured around the 2-D array in terms of the gross characteristics of the flow field. Flow approaching the 3-D building array decelerates more slowly than the flow approaching the 2-D array, although the depth over which the deceleration takes place is essentially the same (about 1H) in both cases. The upstream reverse flow region is smaller for the 3-D case, extending to about 0.25H upstream and 0.1H in the vertical, as opposed to about 0.5H upstream and 0.25H in the vertical for the 2-D array. At higher elevations (1.5-3H), the flow over the 2-D array clearly accelerates, but little, if any, acceleration is apparent for the 3-D array. Flow over top of the first building of the 3-D array shows separation taking place, albeit rather shallow compared to the 2-D array. Indeed, at 0.1H above the first building in the 3-D array, there is no mean reverse flow, whereas the 2-D array showed a mean reverse flow over the entire top of the building at that height. Velocity profiles in the canyons downstream of the buildings are essentially identical for the 3-D array. The longitudinal velocity component shows reverse flow to a height of about 0.7H, but the reverse flow near the surface is considerably weaker for the 3-D array than for the 2-D array. Velocity profiles downstream of the 3-D array show reverse flow until approximately 1.2H downstream of the last building, whereas reverse flow extended slightly more than 3.5H downstream of the 2-D array. For both arrays, the velocity profiles farther downstream relax toward their undisturbed values and show little difference between the 2-D and 3-D arrays beyond 5.5H downstream.
The data from this study and the 2-D array measurements are contrasted with results from other field and laboratory studies, and some conclusions are drawn regarding the representativeness of the results for the proposed application.