Weibull-k Revisited: “Tall” Profiles and Height Variation of Wind Statistics
Log wind profile
Roughness length
Shape parameter
DOI:
10.1007/s10546-014-9915-5
Publication Date:
2014-03-18T06:33:36Z
AUTHORS (3)
ABSTRACT
The Weibull distribution is commonly used to describe climatological wind-speed distributions in the atmospheric boundary layer. While vertical profiles of mean wind speed layer have received significant attention, variation shape with height less understood. Previously we derived a probabilistic model based on similarity theory for calculating effects stability and planetary boundary-layer depth upon long-term profiles. However, some applications (e.g. energy estimation) require parameter (k), as well speed. Towards aim improving predictions Weibull- $$k$$ profile, develop expressions profile variance speed, including method extending our wind-profile theory; together these two lead Weibull-shape parameter. Further, an alternate made, basis set forth by Wieringa (Boundary-Layer Meteorol, 1989, Vol. 47, 85–110), connecting newly-corrected corollary perturbed geostrophic-drag Troen Petersen (European Wind Atlas, Risø National Laboratory, Roskilde). Comparing models Weibull-k profiles, new interpretation explanation given distributions. Results modelling are shown number sites, discussion models’ efficacy applicability. latter includes comparative evaluation Wieringa-type empirical perturbed-geostrophic forms regard surface-layer behaviour, heights where variability not dominated surface effects.
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