Abstract:
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Wind farms have suffered a spectacular growth in Europe in the last few decades. However, future
changes in climate could affect the availability of the wind resource in certain regions. This work assesses
the capabilities of a Regional Climate Model (WRF) applied at medium-to-high resolution (10 km, 33
vertical layers) over a particularly complex and vulnerable terrain (North Eastern Iberian Peninsula) to
derive mean wind speed and direction for 1981e2000. The model is able to reproduce geographical wind
patterns, although it generally overemphasises surface wind intensity when compared to individual
observations. Projections of mean wind speed changes for 2031e2050 suggest a decrease in surface wind
intensity. Energy density estimations at 60 m agl (typical hub-height) show that the implications of the
wind speed weakening could affect the preferential areas for the wind farm locations defined at present.
Reductions up to 20% of wind energy density are found already in mid-21st century. Therefore, it is
advisable to derive dynamic methodologies to assess the preferential areas for wind farm locations, not
only considering past-time wind climatologies, but also considering future climate changes in
geographical patterns. Regional Climate Models applied at medium-to-high resolution can be useful for
this purpose. |