Wind patterns on complex terrain measured by the met-mast consists of numerous effects. Complex topology, large scale forcing, instantaneous characteristics, as well as the thermal stratification, play certain significant roles affecting the statistical description on site. These events are recorded in the mast or SCADA data sets, which obsess a certain correlation time and space with the neighboring event and locations. The thermal stratification, incorporated with inhomogeneous terrain topography, contributes to different flow patterns in the representation of wind speed and direction. These physical properties can be captured by utilizing the computational fluid dynamics (CFD) method, By re-sampling these effects, in the statistical manner, the wind regime can be recreated in the three-dimensional domain.
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