4.4 Article

Are Urban-Canopy Velocity Profiles Exponential?

Journal

BOUNDARY-LAYER METEOROLOGY
Volume 164, Issue 3, Pages 337-351

Publisher

SPRINGER
DOI: 10.1007/s10546-017-0258-x

Keywords

Canopy flows; Urban environment; Velocity profiles

Funding

  1. Engineering and Physical Sciences Research Council (EPSRC) [GR/882947/01, EP/K04060X/1]
  2. Natural Environment Research Council (NERC) through their NCAS [R8/H/12/83]
  3. NERC [DST/26/39]
  4. Engineering and Physical Sciences Research Council [EP/K04060X/1] Funding Source: researchfish
  5. EPSRC [EP/K04060X/1] Funding Source: UKRI

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Using analyses of data from extant direct numerical simulations and large-eddy simulations of boundary-layer and channel flows over and within urban-type canopies, sectional drag forces, Reynolds and dispersive shear stresses are examined for a range of roughness densities. Using the spatially-averaged mean velocity profiles these quantities allow deduction of the canopy mixing length and sectional drag coefficient. It is shown that the common assumptions about the behaviour of these quantities, needed to produce an analytical model for the canopy velocity profile, are usually invalid, in contrast to what is found in typical vegetative (e.g. forest) canopies. The consequence is that an exponential shape of the spatially-averaged mean velocity profile within the canopy cannot normally be expected, as indeed the data demonstrate. Nonetheless, recent canopy models that allow prediction of the roughness length appropriate for the inertial layer's logarithmic profile above the canopy do not seem to depend crucially on their (invalid) assumption of an exponential profile within the canopy.

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