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W i nd Measurement    87


                8%

                7%                                 2.0%
               Wind speed error at hub height  5%    1.5%
                6%



                                                        1.0%
                4%

                3%

                2%

                1%

                0%
                   10           20          30          40           50
                                  Lower anemometer height [m]
              FIGURE 6-10 Error in wind speed at 80 m that is computed using wind shear
              based on different quality anemometers at an upper height of 50 m and
              different lower heights. (From Taylor, M., Mackiewicz, P., Brower, M. C.,
              Markus, M., An Analysis of Wind Resource Uncertainty in Energy Production
              Estimates, EWEC, London, 2004.)


                    ment heights, and terrain. Figure 6-9 indicates the impact of
                                                           6
                    measurement uncertainty of the anemometer, and Fig. 6-10
                    indicates the impact of measurement heights. In this case, the
                    upper anemometer is at 60 m and the hub height is 80 m. The
                    conclusion is that a larger difference in height yields higher
                    accuracy of wind speed extrapolation. As indicated by the
                    points annotated in Fig. 6-10, error decreases from about 4.7
                    to about 2.9% as the height of lower anemometer is changed
                    from 50 to 40 m. The error is further decreased to 2.4% when
                    lower anemometer is at a height of 30 m. The reason for higher
                    accuracy is explained by considering the power law for shear
                    in the following format:


                                                                   (6-3)
                          γ = log v 1 − log v 2 / log h 1 − log h 2
              Since γ is estimated from 10-min wind speeds, it is instructive to ob-
              serve that γ is the slope in the log v, log h space. A better estimate of
              the slope is achieved when the two measurement points are separated.
              However, there is a limit to the separation in terms of height of the
              lowest anemometer. At some point, the uncertainty in readings of the
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