The near-neutral atmospheric surface layer: turbulence and non-stationarity.
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.
Metzger
M
M
Department of Mechanical Engineering, University of Utah, Salt Lake City, UT 84112, USA. m.metzger@utah.edu
McKeon
B J
BJ
Holmes
H
H