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Turbulence structure in a deciduous forest

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Abstract

Three-dimensional wind velocity components were measured at two levels above and at six levels within a fully-leafed deciduous forest. Greatest shear occurs in the upper 20% of the canopy, where over 70% of the foliage is concentrated. The turbulence structure inside the canopy is characterized as non-Gaussian, intermittant and highly turbulent. This feature is supported by large turbulence intensities, skewness and kurtosis values and by the large infrequent sweeps and ejections that dominate tangential momentum transfer. Considerable day/night differences were observed in the vertical profiles of the mean streamwise wind velocity and turbulence intensities since the stability of the nocturnal boundary layer dampens turbulence above and within the canopy.

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Authors and Affiliations

  1. Atmospheric Turbulence and Diffusion Division/NOAA/ARL, P.O. Box 2546, 37831, Oak Ridge, TN, USA

    Dennis D. Baldocchi & Tilden P. Meyers

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  1. Dennis D. Baldocchi
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  2. Tilden P. Meyers
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Baldocchi, D.D., Meyers, T.P. Turbulence structure in a deciduous forest. Boundary-Layer Meteorol 43, 345–364 (1988). https://doi.org/10.1007/BF00121712

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  • DOI: https://doi.org/10.1007/BF00121712

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