The near-neutral atmospheric surface layer: turbulence and non-stationarity
M Metzger, B.J McKeon, H Holmes
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Source: Crossref
Published: Jan 16, 2007
DOI: 10.1098/rsta.2006.1946
Open original source ↗Source abstract
The neutrally stable atmospheric surface layer is used as a physical model of a very high Reynolds number, canonical turbulent boundary layer. Challenges and limitations with this model are addressed in detail, including the inherent thermal stratification, surface roughness and non-stationarity of the atmosphere. Concurrent hot-wire and sonic anemometry data acquired in Utah's western desert provide insight to Reynolds number trends in the axial velocity statistics and spectra.
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