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Wind field simulations at Askervein hill - WindSim

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As can be seen on figure 3.17, the inflow n°2 seems not to change the results a lot.<br />

On the contrary, the non equilibrium boundary condition seems to yield unphysical solution<br />

on the lee side (see figure 3.18). This boundary condition seems not to fit the case.<br />

3.4. Turbulence model<br />

In this part, different turbulence models are tested : standard k-ε model, modified k-ε model,<br />

mixing length model and two-scale k-ε model.<br />

The c grid is chosen, boundary condition on the ground is GRND2, inflow is the log law<br />

profile.<br />

A line<br />

2.0<br />

1.5<br />

exp results<br />

k−eps mod<br />

2 scale k−eps<br />

mix length<br />

normalized velocity<br />

1.0<br />

0.5<br />

0.0<br />

500.0 1000.0 1500.0 2000.0 2500.0<br />

distance along A line (m)<br />

Figure 3.17. A line with different models<br />

Figures 3.17, 3.18 and 3.19 : The mixing length model yields r<strong>at</strong>her good results along A line<br />

but underpredicts velocities along AA line. The modified constants in the k-ε model do not<br />

seem to improve the results in comparison with the standard values (is th<strong>at</strong> a mistake in the<br />

simul<strong>at</strong>ion parameters ?), whereas the two-scale k-ε model, as expected, slightly improves<br />

results on the lee side, predicting the same results as the k-ε model upwind the <strong>hill</strong> top.<br />

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