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Micro- and macro-dispersive fluxes in canopy flows

Publication ,  Journal Article
Poggi, D; Katul, GG
Published in: Acta Geophysica
January 1, 2008

Resolving every detail of the three-dimensional canopy morphology and its underlying topography remains untenable when modeling high Reynolds number geophysical flows. How to represent the effects of such a complex morphological variability and any concomittant topographic variability into one-dimensional bulk flow representation remains a fundamental challenge to be confronted in canopy turbulence research. Theoretically, planar averaging to the scale of interest should be applied to the time-averaged mean momentum balance; however, such averaging gives rise to covariance or dispersive terms produced by spatial correlations of time-averaged quantities that remain 'unclosed' or require parameterization. When the averaging scale is commensurate with few canopy heights, these covariances can be labeled as 'micro-dispersive' stresses. When averaging is intended to eliminate low-wavenumber topographic variations, we refer to these covariances as 'macro-dispersive' terms. Two flume experiments were used to explore the magnitude and sign of both micro- and macro-dispersive fluxes relative to their conventional Reynolds stresses counterparts: a rod-canopy with variable roughness density and a dense rod canopy situated on gentle hilly terrain. When compared to the conventional momentum flux, the micro-dispersive fluxes in the lowest layers of sparse canopies can be significant (=50%). For dense canopies, the dispersive terms remain negligible when compared to the conventional momentum fluxes throughout. For the macro-dispersive fluxes, model calculations suggest that these terms can be neglected relative to the Reynolds stresses for a deep canopy situated on a narrow hill. For the region in which topographic variations can interact with the pressure, both model calculations and flume experiments suggest that the macro-dispersive fluxes cannot be neglected, and their value can be 20% of the typical Reynolds stresses. © Versita Warsaw and Springer-Verlag Berlin Heidelberg 2008.

Duke Scholars

Published In

Acta Geophysica

DOI

EISSN

1895-7455

ISSN

1895-6572

Publication Date

January 1, 2008

Volume

56

Issue

3

Start / End Page

778 / 799

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3706 Geophysics
  • 3705 Geology
  • 0404 Geophysics
 

Citation

APA
Chicago
ICMJE
MLA
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Poggi, D., & Katul, G. G. (2008). Micro- and macro-dispersive fluxes in canopy flows. Acta Geophysica, 56(3), 778–799. https://doi.org/10.2478/s11600-008-0029-7
Poggi, D., and G. G. Katul. “Micro- and macro-dispersive fluxes in canopy flows.” Acta Geophysica 56, no. 3 (January 1, 2008): 778–99. https://doi.org/10.2478/s11600-008-0029-7.
Poggi D, Katul GG. Micro- and macro-dispersive fluxes in canopy flows. Acta Geophysica. 2008 Jan 1;56(3):778–99.
Poggi, D., and G. G. Katul. “Micro- and macro-dispersive fluxes in canopy flows.” Acta Geophysica, vol. 56, no. 3, Jan. 2008, pp. 778–99. Scopus, doi:10.2478/s11600-008-0029-7.
Poggi D, Katul GG. Micro- and macro-dispersive fluxes in canopy flows. Acta Geophysica. 2008 Jan 1;56(3):778–799.
Journal cover image

Published In

Acta Geophysica

DOI

EISSN

1895-7455

ISSN

1895-6572

Publication Date

January 1, 2008

Volume

56

Issue

3

Start / End Page

778 / 799

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3706 Geophysics
  • 3705 Geology
  • 0404 Geophysics