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Figure 6: CW wind lidars (ZephIRs) under testing at Høvsøre, Risø <strong>DTU</strong><br />

Figure 7: Pulsed wind lidars (six WLS7 WindCubes) and one Galion (far back) during testing<br />

at Høvsøre, Risø <strong>DTU</strong><br />

1.3.4 Wind profiling<br />

A wind “profiler” measures 10-min averaged quantities of the vertical wind speed profile, the<br />

vertical direction profile, and the vertical turbulence profiles, by combining a series of radial<br />

measured wind speed components from several, and at least three, different beam directions,<br />

into a three-dimensional wind vector. CW-based wind lidars, e.g. the ZephIR, measure the<br />

vertical wind profile at five consecutive heights, selectable in the range from, say 10 to 150 m<br />

height. Pulsed lidars, e.g. the WindCube or the Galion, measure correspondingly the vertical<br />

wind profile simultaneously at several (of the order of 10) heights, in the height interval from<br />

40–∼ 300 m, the upper bound depending on the amount of aerosols in the air.<br />

True for all wind profilers in the wind energy market, however, CW and pulsed lidars<br />

irrespectively, is that they rely during combining measured radial wind speeds into a single<br />

wind vector on the assumption that the flow over the wind lidar is strictly homogeneous.<br />

Homogeneous wind flow means that the air stream is unaffected and not influenced by hills,<br />

<strong>DTU</strong> Wind Energy-E-Report-0029(EN) 21

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