wind energy resource evaluation in a site of central italy ... - WindSim
wind energy resource evaluation in a site of central italy ... - WindSim
wind energy resource evaluation in a site of central italy ... - WindSim
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Analyz<strong>in</strong>g RMS error table for tower 5424, it is found that the sectors whereturbulence <strong>in</strong>tensity level is higher is 240°, dur<strong>in</strong>g both periods April-May andNovember-December. Sectors where turbulence <strong>in</strong>tensity is lower are sector 180°and 60°, respectively for periods April-May and November-December. Byconsider<strong>in</strong>g the RMS table and the U30 table, different behaviors for the twoperiods <strong>of</strong> reference can be found. In fact, dur<strong>in</strong>g April-May the error seems to<strong>in</strong>crease with the <strong>w<strong>in</strong>d</strong> speed, while dur<strong>in</strong>g November –December the error seemsto decrease when U30 is grow<strong>in</strong>g. This behavior is well represented by the trendl<strong>in</strong>es shown <strong>in</strong> figure 6.7.In general, it can be stated that the values <strong>of</strong> the T.I. seem to be strongly l<strong>in</strong>ked tothe seasonal thermal effects. As was already said before, the solar radiation and thethermal <strong>in</strong>ertia <strong>of</strong> the terra<strong>in</strong> can generate different <strong>w<strong>in</strong>d</strong> breezes <strong>in</strong> themeasurement periods, also <strong>in</strong>fluenc<strong>in</strong>g the turbulence level. A stronger <strong>in</strong>fluence onthe turbulence <strong>in</strong>tensity level can be due also to the orographic effects. The tower5424 is placed <strong>in</strong> a cliff, where vertical component <strong>of</strong> velocity are present and can bestrongly variable <strong>in</strong> <strong>in</strong>tensity dur<strong>in</strong>g the whole year because <strong>of</strong> the different solarradiation. Particularly, strong solar radiation near a cliff can generate a <strong>in</strong>tensevertical <strong>w<strong>in</strong>d</strong>, where the fluctuations are stronger. This phenomenon could expla<strong>in</strong>the trend relative to April-May period <strong>in</strong> figure 6.7, where <strong>in</strong> general the errors<strong>in</strong>crease with the U30.F<strong>in</strong>ally, it must be said that turbulence is a parameter very difficult to measure,especially <strong>in</strong> atmospheric flows, and that a only a longer measurement campaigncan guarantee more accurate results. Due to all this consideration, the agreementbetween experimental data and CFD results for mast 5424 was fairly good.104