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- W2990431717 abstract "Theprobabilitydensityfunction(pdf)oflandsurfacewindspeedsischaracterizedusingaglobalnetworkof observations. Daytime surface wind speeds are shown to be broadly consistent with the Weibull distribution, while nighttime surface wind speeds are generally more positively skewed than the corresponding Weibull distribution (particularly in summer). In the midlatitudes, these strongly positive skewnesses are shown to be generally associated with conditions of strong surface stability and weak lower-tropospheric wind shear. Long-term tower observations from Cabauw, the Netherlands, and Los Alamos, New Mexico, demonstrate that lower-tropospheric wind speeds become more positively skewed than the corresponding Weibull distribution only in the shallow (;50 m) nocturnal boundary layer. This skewness is associated with two populations of nighttime winds: (i) strongly stably stratified with strong wind shear and (ii) weakly stably or unstably stratified with weak wind shear. Using an idealized two-layer model of the boundary layer momentumbudget,itisshownthattheobservedvariabilityofthedaytimeandnighttimesurfacewindspeedscan be accounted for through a stochastic representation of intermittent turbulent mixing at the nocturnal boundary layer inversion." @default.
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- W2990431717 date "2011-12-01" @default.
- W2990431717 modified "2023-09-26" @default.
- W2990431717 title "The Probability Distribution of Land Surface Wind Speeds" @default.
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