Two-Dimensional Scalar Spectra in the Deeper Layers of a Dense and Uniform Model Canopy
Authors: Poggi, D.; Katul, G.
Source: Boundary-Layer Meteorology, Volume 121, Number 2, November 2006 , pp. 267-281(15)
Publisher: Springer
Abstract:
The turbulent flow inside dense canopies is characterized by wake production and short-circuiting of the energy cascade. How these processes affect passive scalar concentration variability in general and their spectral properties in particular remains a vexing problem. Progress on this problem is frustrated by the shortage of high resolution spatial concentration measurements, and by the lack of simplified analytical models that connect spectral modulations in the turbulent kinetic energy (TKE) cascade to scalar spectra. Here, we report the first planar two-dimensional scalar concentration spectra (Φ cc ) inside tall canopies derived from flow visualization experiments. These experiments were conducted within the deeper layers of a model canopy composed of densely arrayed cylinders welded to the bottom of a large recirculating water channel. We found that in the spectral region experiencing wake production, the Φ cc exhibits directional scaling power laws. In the longitudinal direction (x), or the direction experiencing the largest drag force, the Φ cc (k x ) was steeper than <EquationSource Format="TEX"><![CDATA[$$k_x^{-5/3}$$]]></EquationSource> and followed an approximate <EquationSource Format="TEX"><![CDATA[$$k_x^{-7/3}$$]]></EquationSource> at wavenumbers larger than the injection scale of wake energy, where k x is the longitudinal wavenumber. In the lateral direction (y), the spectra scaled as <EquationSource Format="TEX"><![CDATA[$$k_y^{-5/3}$$]]></EquationSource> up to the injection scale, and then decayed at an approximate <EquationSource Format="TEX"><![CDATA[$$k_y^{-7/3}$$]]></EquationSource> power law. This departure from the classical inertial subrange scaling (i.e., k −5/3) was reproduced using a newly proposed analytical solution to a simplified scalar spectral budget equation. Near the velocity viscous dissipation range, the scalar spectra appear to approach an approximate k −3, a tantalizing result consistent with dimensional analysis used in the inertial-diffusive range. Implications to subgrid modelling for large-eddy simulations (LES) inside canopies are briefly discussed.Keywords: Canopy turbulence; Laser-induced fluorescence technique; Two-dimensional scalar spectra; Wake production
Document Type: Research article
DOI: http://dx.doi.org/10.1007/s10546-006-9075-3
Affiliations: 1: Email: gaby@duke.edu
Publication date: 2006-11-01
- In this: publication
- By this: publisher
- In this Subject: Geophysics & Geomagnetism , Meteorology & Climatology , Hydraulic & Environmental Engineering
- By this author: Poggi, D. ; Katul, G.

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