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Volume 119, Issue 513 pp. 1071-1104
Article

Turbulent transfer relationships over an urban surface. I. Spectral characteristics

M. Roth

Corresponding Author

M. Roth

University of British Columbia, Canada

Atmospheric Science Programme, Department of Geography, University of British Columbia, Vancouver, B.C., CanadaSearch for more papers by this author
T. R. Oke

T. R. Oke

University of British Columbia, Canada

Search for more papers by this author
First published: July 1993 Part B
Citations: 13

Abstract

A comprehensive study of atmospheric turbulence over an urban surface has been carried out. In this Part I of the study the spectral characteristics are analysed. Results involving all the important atmospheric variables, Measured at two heights (z'/z0=21 and 37) under unstable conditions, are presented, normalized by the respective variances/covariances, and within the Monin-Obukhov similarity framework. Although the shapes and location of the peaks of the urban spectra/cospectra are in good agreement with homogeneous surface layer data, the analysis of the normalized dissipation rates and spectral correlation coefficients reveals differences which can be attributed to the rough surface. For example, the dissipation of turbulent kinetic energy is relatively small, perhaps owing to an increase in the transport and export of locally produced turbulent energy; there is a very efficient transfer of Momentum which it is suggested may be a result of wake production associated with bluff bodies, and it is found that the transfer of heat and moisture are dissimilar.