Modification to the law of the wall represented by a dimensionless correction function ϕRSL(z/h) is derived using atmospheric turbulence measurements collected at two sites in the Amazon in near-neutral stratification, where z is the distance from the forest floor and h is the mean canopy height. The sites are the Amazon Tall Tower Observatory for z/h∈ [1,2.3] and the Green Ocean Amazon (GoAmazon) site for z/h∈ [1,1.4]. Here, a link between the vertical velocity spectrum Eww(k) (k is the longitudinal wavenumber) and ϕRSL is then established using a co-spectral budget (CSB) model interpreted by the moving-equilibrium hypothesis. The key finding is that ϕRSL is determined by the ratio of two turbulent viscosities and is given as νt,BL/νt,RSL, where νt,RSL = (1/A)∫$$^{∞}_{0}$$ τ(k)Eww(k)dk, νt,BL = kv(z−d)u*, τ(k) is a scale-dependent decorrelation time scale between velocity components, A = CR/(1−CI) = 4.5 is predicted from the Rotta constant CR = 1.8, and the isotropization of production constant CI = 3/5 given by rapid distortion theory, kv is the von Kármán constant, u* is the friction velocity at the canopy top, and d is the zero-plane displacement. Because the transfer of energy across scales is conserved in Eww(k) and is determined by the turbulent kinetic energy dissipation rate (ε), the CSB model also predicts that ϕRSL scales with LBL/Ld, where LBL is the length scale of attached eddies to z = d, and Ld = u$$_{*}^{3}$$/ε is a macro-scale dissipation length.
Mortarini, Luca, et al. "Adjustments to the law of the wall above an Amazon forest explained by a spectral link." Physics of Fluids, vol. 35, no. 2, Feb. 2023. https://doi.org/10.1063/5.0135697
Mortarini, Luca, Katul, Gabriel G., Cava, Daniela, Dias-Junior, Cleo Quaresma, Dias, Nelson Luis, Manzi, Antonio, Sorgel, Matthias, Araújo, Alessandro, & Chamecki, Marcelo (2023). Adjustments to the law of the wall above an Amazon forest explained by a spectral link. Physics of Fluids, 35(2). https://doi.org/10.1063/5.0135697
Mortarini, Luca, Katul, Gabriel G., Cava, Daniela, et al., "Adjustments to the law of the wall above an Amazon forest explained by a spectral link," Physics of Fluids 35, no. 2 (2023), https://doi.org/10.1063/5.0135697
@article{osti_2903805,
author = {Mortarini, Luca and Katul, Gabriel G. and Cava, Daniela and Dias-Junior, Cleo Quaresma and Dias, Nelson Luis and Manzi, Antonio and Sorgel, Matthias and Araújo, Alessandro and Chamecki, Marcelo},
title = {Adjustments to the law of the wall above an Amazon forest explained by a spectral link},
annote = {Modification to the law of the wall represented by a dimensionless correction function ϕRSL(z/h) is derived using atmospheric turbulence measurements collected at two sites in the Amazon in near-neutral stratification, where z is the distance from the forest floor and h is the mean canopy height. The sites are the Amazon Tall Tower Observatory for z/h∈ [1,2.3] and the Green Ocean Amazon (GoAmazon) site for z/h∈ [1,1.4]. Here, a link between the vertical velocity spectrum Eww(k) (k is the longitudinal wavenumber) and ϕRSL is then established using a co-spectral budget (CSB) model interpreted by the moving-equilibrium hypothesis. The key finding is that ϕRSL is determined by the ratio of two turbulent viscosities and is given as νt,BL/νt,RSL, where νt,RSL = (1/A)∫$^{∞}_{0}$ τ(k)Eww(k)dk, νt,BL = kv(z−d)u*, τ(k) is a scale-dependent decorrelation time scale between velocity components, A = CR/(1−CI) = 4.5 is predicted from the Rotta constant CR = 1.8, and the isotropization of production constant CI = 3/5 given by rapid distortion theory, kv is the von Kármán constant, u* is the friction velocity at the canopy top, and d is the zero-plane displacement. Because the transfer of energy across scales is conserved in Eww(k) and is determined by the turbulent kinetic energy dissipation rate (ε), the CSB model also predicts that ϕRSL scales with LBL/Ld, where LBL is the length scale of attached eddies to z = d, and Ld = u$_{*}^{3}$/ε is a macro-scale dissipation length.},
doi = {10.1063/5.0135697},
url = {https://www.osti.gov/biblio/2903805},
journal = {Physics of Fluids},
issn = {ISSN 1070-6631},
number = {2},
volume = {35},
place = {United States},
publisher = {AIP Publishing},
year = {2023},
month = {02}}
ARM Data Center, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States); University of California, Los Angeles, CA (United States)
Sponsoring Organization:
Brazilian Ministério da Ciência, Tecnologia e Inovação; German Federal Ministry of Education and Research; Instituto Nacional de Pesquisas da Amazônia (INPA); Max-Planck Society; National Science Foundation; U.S. National Science Foundation; USDOE; USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
SC0011075; SC0022072
OSTI ID:
2903805
Alternate ID(s):
OSTI ID: 1922976 OSTI ID: 1957725
Journal Information:
Physics of Fluids, Journal Name: Physics of Fluids Journal Issue: 2 Vol. 35; ISSN 1089-7666; ISSN 1070-6631