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wind energy resource evaluation in a site of central italy ... - WindSim

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As it can be seen from figures number 2.5 and 2.6, the <strong>in</strong>crease <strong>of</strong> the heightdistribution factor seems to be not responsible <strong>of</strong> the variation <strong>of</strong> the verticalpr<strong>of</strong>iles. Anyhow, a better accuracy <strong>of</strong> the results is obta<strong>in</strong>ed, as a general rule, forlow values <strong>of</strong> the HDF, which moves the vertical <strong>central</strong> cell po<strong>in</strong>ts <strong>in</strong> a region closerto the ground, where velocity gradients are higher.Figure 2.7: Zoom <strong>of</strong> the figure 2.5.Figure 2.6 shows that the three curves don’t overlap completely, as it can be seenalso from the zoom <strong>in</strong> the further figure 2.7.The phenomenon shown <strong>in</strong> figure 2.7 is very important, and must be taken <strong>in</strong>toaccount when work<strong>in</strong>g with <strong>w<strong>in</strong>d</strong> data measured at low height respect to the groundlevel. So it’s reasonable to run simulations with low values <strong>of</strong> height distributionfactor when a particular precision near the ground level is needed, while <strong>in</strong>situations regard<strong>in</strong>g the <strong>evaluation</strong> <strong>of</strong> the <strong>w<strong>in</strong>d</strong> <strong>resource</strong>s at high levels thisphenomenon becomes less marked. The experience shows, moreover, that theheight distribution factor cannot be decreased <strong>in</strong>def<strong>in</strong>itely, but its value is strictlyconnected to the resolution <strong>of</strong> the horizontal grid. Then, if it is necessary to havegood precision <strong>in</strong> such low heights, also the dimension <strong>of</strong> the horizontal cells must21

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