The near-neutral atmospheric surface layer: turbulence and non-stationarity-Reference-Cited by-同舟云学术

The near-neutral atmospheric surface layer: turbulence and non-stationarity

Published:2007-01-16 Issue:1852 Volume:365 Page:859-876
ISSN:1364-503X
Container-title:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
language:en
Short-container-title:Phil. Trans. R. Soc. A.

Author:

Metzger M¹,McKeon B.J²,Holmes H¹

Affiliation:

1. Department of Mechanical Engineering, University of UtahSalt Lake City, UT 84112, USA

2. Graduate Aeronautical Laboratories, California Institute of TechnologyPasadena, CA 91125, USA

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.

Publisher

The Royal Society

Subject

General Physics and Astronomy,General Engineering,General Mathematics

Link

https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2006.1946

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