Abstract
This study attempts to determine the scales of turbulence in a high Reynolds number shear flow near which transition to isotropy occurs and the scales for which Taylor's hypothesis is applicable. The flow studied was the wind near height x 3 = 2 m above a flat land surface. Four hot-wire anemometers were mounted in a three-dimensional array with equal separations between 1.8 m and 2 cm in three different directions. Theoretical cross-spectra were computed from the observed spectra of downwind velocity fluctuations assuming isotropy and Taylor's hypothesis. Comparison between these and the observed cross-spectra revealed that the turbulence in the flow studied was consistent with both assumptions provided k 1x3&> 20, where k 1 is the radian wavenumber; this was the lower bound to which no departure from isotropy could be detected by the experiment. For 4 ≦ k 1x3≦ 20, the observations are consistent with symmetry of the turbulence about the downstream direction. That part of Taylor's hypothesis relating observed frequency at a stationary sensor to the downstream wavenumber component appears to be justified within experimental error for k 1x3& > 3.
Similar content being viewed by others
References
Busch, N. E.: 1973, ‘The Surface Boundary Layer’, Boundary-Layer Meteorol. 4, 213–240.
Champagne, F.: 1978, ‘The Fine-Scale Structure of the Turbulent Velocity Field’, J. Fluid. Mech. 86, 67–108.
Hinze, J. O.: 1959, Turbulence, McGraw-Hill Book Co, New York, 586 pp.
Kaimal, J. C., Wyngaard, J. C., Izumi, Y., and Coté, O. R.: 1972, ‘Spectral Characteristics of Surface Layer Turbulence’, Quart. J. Roy. Meteorol. Soc. 98, 563–589.
Lumley, J. L. and Panofsky, H. A.: 1964, The Structure of Atmospheric Turbulence, Interscience-Wiley, 239 pp.
Pond, S., Stewart, R. W., and Burling, R. W.: 1963, ‘Turbulence Spectra in the Wind Over Waves’, J. Atmos. Sci. 20, 319–324.
Webster, I.: 1972, ‘A Study of Isotropic Structure in Atmospheric Boundary-Layer Turbulence’, M.Sc. thesis, University of British Columbia, Vancouver, Canada.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Webster, I.T., Burling, R.W. A test of isotropy and Taylor's hypothesis in the atmospheric boundary layer. Boundary-Layer Meteorol 20, 429–443 (1981). https://doi.org/10.1007/BF00122293
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1007/BF00122293