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

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5.3 Microscale model – evidence <strong>of</strong> recirculationThe small variations highlighted <strong>in</strong> the mesoscale model for sector 90, placed <strong>in</strong> thewest region <strong>of</strong> the <strong>site</strong>, led to a need for a deeper study <strong>in</strong> order to understand thecauses that generate the differences <strong>in</strong> speed-up. A wise preview <strong>of</strong> thephenomenon can be done consider<strong>in</strong>g the specified <strong>w<strong>in</strong>d</strong> direction and theorography map, shown <strong>in</strong> chapter 4 In fact, a deep valley is present <strong>in</strong> the west zone<strong>of</strong> the <strong>site</strong>, correspond<strong>in</strong>g to the path <strong>of</strong> the roads signed <strong>in</strong> the map. In this region arecirculation effect due to high steepness <strong>of</strong> the west-side <strong>of</strong> the mounta<strong>in</strong> can begenerated when the <strong>w<strong>in</strong>d</strong> is blow<strong>in</strong>g from the east direction.A smaller model has been created and the orography map is shown <strong>in</strong> the follow<strong>in</strong>gpicture 5.3.Figure 5.3: Orographic 3D map <strong>of</strong> the microscale model.The microscale model covers an area <strong>of</strong> dimensions 6 X 6 km and has a gridresolution f<strong>in</strong>er than the mesoscale model previously described. Boundaryconditions are superimposed by the outer model (nest<strong>in</strong>g technique).The general parameters applied <strong>in</strong> the simulation, run for <strong>w<strong>in</strong>d</strong> direction 90 degreesand <strong>w<strong>in</strong>d</strong> speed 10 m/s, are exposed <strong>in</strong> the tables 5.3 and 5.4.77

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