An investigation of higher-order closure models for a forested canopy

• Published in: Boundary-layer meteorology Vol. 89; no. 1; pp. 47 - 74
• Main Authors: Katul, G.G. (Duke Univ., Durham, NC (USA). School of Environment), Albertson, J.D
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer 01.10.1998; Springer Nature B.V
• Subjects: Atmospheric boundary layer; ATMOSPHERIC DISTURBANCES; BOSQUES; CANOPY; Convection, turbulence, diffusion. Boundary layer structure and dynamics; COUVERT; CUBIERTA DE COPAS; Earth, ocean, space; Exact sciences and technology; External geophysics; FENOMENOS ATMOSFERICOS; FORESTS; FORET; Meteorology; MODELE; MODELOS; PERTURBATION ATMOSPHERIQUE; PINUS; VELOCIDAD; VELOCITY; VENT; VIENTO; VITESSE; WINDS; North Carolina; United States; North America; America; Reynolds stress; Closure model; Parametrization; Forests; Atmospheric turbulence; Atmospheric boundary layer; Vertical profile; Algorithm; Anemometry
• ISSN: 0006-8314; 1573-1472
• DOI: 10.1023/A:1001509106381

Simultaneous triaxial sonic anemometer velocity measurements vertically arrayed at six levels within and above a uniform pine forest were used to examine two parameterization schemes for the triple-velocity correlation tensor employed in higher-order closure models. These parameterizations are the gradient-diffusion approximation typically used in second-order closure models, and the full budget for the triple-velocity correlation tensor typically employed in third-order closure models. Both second- and third-order closure models failed to reproduce the measured profiles of the triple-velocity correlation within and above the canopy. However, the Reynolds stress tensor profiles (including velocity variances) deviated greatly from the measurements only within the lower levels of the canopy. It is shown that the Reynolds stresses are most sensitive to the parameterization of the triple-velocity correlation in these lower canopy regions where local turbulent production is negligible and turbulence is mainly sustained by the flux transport term. The failure of the third-order closure model to reproduce the measured third moments in the upper layers of the canopy-top contradicts conclusions from a previous study over shorter vegetation but agrees with another study for a deciduous forest. Whether the third-order closure model failure is due to the zero-fourth-cumulant closure approximation is therefore considered. Comparisons between measured and predicted quadruple velocity correlations suggest that the zero-fourth-cumulant approximation is valid close to the canopy-atmosphere in agreement with recent experiments.[PUBLICATION ABSTRACT]