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Momentum Transfer and Turbulent Kinetic Energy Budgets within a Dense Model Canopy

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Abstract

Second-order closure models for the canopy sublayer (CSL) employ aset of closure schemes developed for `free-air' flow equations andthen add extra terms to account for canopy related processes. Muchof the current research thrust in CSL closure has focused on thesecanopy modifications. Instead of offering new closure formulationshere, we propose a new mixing length model that accounts for basicenergetic modes within the CSL. Detailed flume experiments withcylindrical rods in dense arrays to represent a rigid canopy areconducted to test the closure model. We show that when this lengthscale model is combined with standard second-order closureschemes, first and second moments, triple velocity correlations,the mean turbulent kinetic energy dissipation rate, and the wakeproduction are all well reproduced within the CSL provided thedrag coefficient (CD) is well parameterized. The maintheoretical novelty here is the analytical linkage betweengradient-diffusion closure schemes for the triple velocitycorrelation and non-local momentum transfer via cumulant expansionmethods. We showed that second-order closure models reproducereasonably well the relative importance of ejections and sweeps onmomentum transfer despite their local closure approximations.Hence, it is demonstrated that for simple canopy morphology (e.g.,cylindrical rods) with well-defined length scales, standard closureschemes can reproduce key flow statistics without much revision.When all these results are taken together, it appears that thepredictive skills of second-order closure models are not limitedby closure formulations; rather, they are limited by our abilityto independently connect the drag coefficient and the effectivemixing length to the canopy roughness density. With rapidadvancements in laser altimetry, the canopy roughness densitydistribution will become available for many terrestrialecosystems. Quantifying the sheltering effect, the homogeneity andisotropy of the drag coefficient, and more importantly, thecanonical mixing length, for such variable roughness density isstill lacking.

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Authors and Affiliations

  1. Dipartimento di Idraulica, Trasporti ed Infrastrutture Civili Politecnico di Torino, Torino, Italy &

    D. Poggi

  2. Department of Civil and Environmental Engineering, Duke University, Durham, North Carolina, U.S.A

    D. Poggi

  3. Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina, U.S.A

    G. G. Katul

  4. Department of Civil and Environmental Engineering, Duke University, Durham, North Carolina, U.S.A

    J. D. Albertson

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  1. D. Poggi
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  2. G. G. Katul
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  3. J. D. Albertson
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Poggi, D., Katul, G.G. & Albertson, J.D. Momentum Transfer and Turbulent Kinetic Energy Budgets within a Dense Model Canopy. Boundary-Layer Meteorology 111, 589–614 (2004). https://doi.org/10.1023/B:BOUN.0000016502.52590.af

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