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42 J.C.L. da Costa et al.<br />

y/h<br />

1.5<br />

1<br />

0.5<br />

2 x/h=0.02 0.25 0.55<br />

1.2 2.6 6.5 13.2 21.8<br />

0<br />

0 2 4 6 0 2 4 6 0 2 4 6 0 2 4 6 0 2 4 6 0 2 4 6 0 2 4 6 0 2 4 6<br />

u (m/s)<br />

Fig. 7.3. Longitudinal velocity along a forest clearing. <strong>Wind</strong> tunnel data (dashed<br />

line, solid line); Svensson [6] (dashed line), Liu [4] (solid line), v2-f model (dotted<br />

line)<br />

Concerning the mean velocity (Fig. 7.3), all models show a much better<br />

agreement with the wind tunnel data, compared with Fig. 7.2.<br />

7.4 Conclusions<br />

There are difficulties in the computer simulation of wind flow over forests,<br />

related with model parameterisation, which require the availability of good<br />

experimental data.<br />

References<br />

1. F.A.Castro,J.M.L.M.Palma,andA.SilvaLopes.SimulationoftheAskervein<br />

flow. Part 1: Reynolds averaged Navier-Stokes equations (k-ɛ turbulence model).<br />

Boundary-Layer Meteorol., 107:501–530, 2003<br />

2. G. G. Katul, L. Mahrt, D. Poggi, and Christophe Sanz. One- and two-equation<br />

models for canopy turbulence. Boundary-Layer Meteorol., 113:81–109, 2004<br />

3. F. S. Lien and P. A. Durbin. Non-linear k–ε − v modeling with application to<br />

high-lift. In Proc of the Summer Program. CTR, Stanford University, 1996<br />

4. J. Liu, J. M. Chen, T. A. Black, and M. D. Novak. E–ε modelling of turbulent<br />

air flow downwind of a model forest edge. Boundary-Layer Meteorol., 77:21–44,<br />

1996<br />

5. B. Ruck and E. Adams. Fluid mechanical aspects in the pollutants transport to<br />

coniferous trees. Boundary-Layer Meteorol., 56:163–195, 1991<br />

6. U. Svensson and K. Häggkvist. A two-equation turbulence model for canopy<br />

flows. J. <strong>Wind</strong> Eng. Ind. Aerodyn., 35:201–211, 1990

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