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Optimization and Computational Fluid Dynamics - Department of ...

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2 A Few Illustrative Examples <strong>of</strong> CFD-based <strong>Optimization</strong> 51<br />

0.9<br />

0.8<br />

0.7<br />

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0.3<br />

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0.1<br />

0<br />

Wilcox (1998)<br />

β0 β ∗ 0 σ σ ∗ α<br />

Fig. 2.20 The five input parameters <strong>of</strong> the optimization represented using parallel coordinates<br />

corresponding values in Fig. 2.20. The original values proposed by Wilcox<br />

[79] are also represented in this figure with symbols.<br />

Figure 2.20 also shows that considerable modifications <strong>of</strong> the model parameters<br />

have been tested by the optimization procedure, compared to the<br />

original reference values proposed by Wilcox [79].<br />

A total <strong>of</strong> 5,050 evaluations have been performed during the optimization<br />

procedure. Plotting two arbitrary objectives (i.e., the errors for two different<br />

Reynolds numbers) against each other, a strong linear dependence can be<br />

observed (Fig. 2.21). This is satisfactory, since it demonstrates that, globally,<br />

a good parameter set will be valid for different Reynolds numbers, which is<br />

essential for practical purposes. However, zooming on the best results (lower<br />

left corner) in order to see the details, a Pareto front corresponding to concurrent<br />

objectives is detected (Fig. 2.22). This proves that one single, optimal<br />

parameter set cannot be found that would be equally valid for all Reynolds<br />

numbers.<br />

The computed velocity pr<strong>of</strong>iles using the model constants in one optimum<br />

configuration are shown in Fig. 2.23. These pr<strong>of</strong>iles are compared to DNS data<br />

<strong>and</strong> to the results computed with the original parameter values. The proposed<br />

modifications lead to a considerably better agreement with the DNS.<br />

Figure 2.24 finally shows the four objectives <strong>of</strong> the optimization compared<br />

with results obtained by the original model ([79], shown with symbols). Parallel<br />

coordinates are used to represent the connection between the corresponding<br />

values. It can be clearly seen that, in all four cases, better results are<br />

obtained with an optimal parameter set compared with the values proposed<br />

by Wilcox in 1998 for channel flows.

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