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Com. Figure 3-14. com. Figure 3-12. Example of strong wind shear. e. so-called negative wind shear. Courtesy Vestas. These are all wind events, which by nature fall outside of what can normally be represented by stationary wind conditions. Note that the simultaneous change in wind direction and wind speed occurs when fronts of extreme gust. g. the 50-year wind speed. The 50-year wind speed is the 10-minute mean wind speed, which, on average, is exceeded once every fifty years. Determination of the 50-year wind speed requires an extreme value 3 – External Conditions 43 Guidelines for Design of Wind Turbines − DNV/Risø analysis of available wind speed data.

100 Wind rose The distribution of the wind direction is of particular interest with respect to installation of turbines in wind farms. 3, wind turbines installed behind obstacles, such as for example other turbines, cause a considerable increase in turbulence intensity. downwind upwind height (m) ridge crest 10 The distribution of the wind direction is often represented by a wind rose as the one seen in Figure 3-10. 1 0 5 10 15 20 wind speed (m/s) Figure 3-8. Wind profiles observed upwind, at the crest, and at the foot downwind of a two-dimensional ridge.

G. over a 10-second period. Extreme wind speeds can be treated in a traditional manner as extremes of the wind speed process during stationary 10-minute conditions. An example of a wind speed record containing extreme gust is given in Figure 3-14. Figure 3-11. Example of extreme rise time for gust. com. Figure 3-14. com. Figure 3-12. Example of strong wind shear. e. so-called negative wind shear. Courtesy Vestas. These are all wind events, which by nature fall outside of what can normally be represented by stationary wind conditions.

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