Abstract
Measurements of longitudinal turbulent velocity were made at pairs of levels inside and above a model plant canopy in the wind tunnel. It was found that above approximately the zero-plane displacement level, the coherence and phase results were similar in many respects to atmospheric data, but that deviations from this behaviour appeared deeper in the model canopy.
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References
Davenport, A. G.: 1961, ‘The Spectrum of Horizontal Gustiness in High Winds’, Quart. J. Roy. Meteorol. Soc. 87, 194–211.
Favre, A. J., Gaviglio, J. J. and Dumas, R.: 1957, ‘Space-Time Correlations and Spectra in a Turbulent Boundary Layer’, J. Fluid Mech. 2, 313–342.
Lumley, J. L. and Panofsky, H. A.: 1964, The Structure of Atmospheric Turbulence, Interscience Monographs and Texts in Physics and Astronomy, Volume XII, John Wiley and Sons, New York, 239 pp.
Naito, G. and Kondo, J.: 1974, ‘Spatial Structure of Fluctuating Components of the Horizontal Wind Speed Above the Ocean’, J. Meteorol. Soc. Japan 52, 391–399.
Pielke, R. A. and Panofsky, H. A.: 1970, ‘Turbulence Characteristics Along Several Towers’, Boundary-Layer Meteorol. 1, 115–130.
Seginer, I., Mulhearn, P. J., Bradley, E. F. and Finnigan, J. J.: 1976, ‘Turbulent Flow in a Model Plant Canopy’, Boundary-Layer Meteorol. 10, 423–453.
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Seginer, I., Mulhearn, P.J. A note on vertical coherence of streamwise turbulence inside and above a model plant canopy. Boundary-Layer Meteorol 14, 515–523 (1978). https://doi.org/10.1007/BF00121891
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DOI: https://doi.org/10.1007/BF00121891