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A spectral and lag-correlation analysis of turbulence in a deciduous forest canopy

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Abstract

The processes influencing turbulence in a deciduous forest and the relevant length and time scales are investigated with spectral and cross-correlation analysis. Wind velocity power spectra were computed from three-dimensional wind velocity measurements made at six levels inside the plant canopy and at one level above the canopy. Velocity spectra measured within the plant canopy differ from those measured in the surface boundary layer. Noted features associated with the within-canopy turbulence spectra are: (a) power spectra measured in the canopy crown peak at higher wavenumbers than do those measured in the subcanopy trunkspace and above the canopy; (b) peak spectral values collapse to a relatively universal value when scaled according to a non-dimensional frequency comprised of the product of the natural frequency and the Eulerian time scale for vertical velocity; (c) at wavenumbers exceeding the spectral peak, the slopes of the power spectra are more negative than those observed in the surface boundary layer; (d) Eulerian length scales decrease with depth into the canopy crown, then increase with further depth into the canopy; (e) turbulent events below crown closure are more correlated with turbulent events above the canopy than are those occurring in the canopy crown; and (f) Taylor's frozen eddy hypothesis is not valid in a plant canopy. Interactions between plant elements and the mean wind and turbulence alter the processes that produce, transport and remove turbulent kinetic energy and account for the noted observations.

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Authors and Affiliations

  1. Atmospheric Turbulence and Diffusion Division, National Oceanic and Atmospheric Administration, Air Resource Laboratory, P.O. Box 2456, 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. A spectral and lag-correlation analysis of turbulence in a deciduous forest canopy. Boundary-Layer Meteorol 45, 31–58 (1988). https://doi.org/10.1007/BF00120814

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