Roof-level large- and small-scale coherent structures in a street canyon flow
The characteristics of large- and small-scale turbulent motions at roof-level in a street canyon flow were experimentally investigated along with their spatio-temporal organization and their mutual interaction in this region. Quadrant analysis was conducted to identify sweep and ejection events, whi...
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Veröffentlicht in: | Environmental fluid mechanics (Dordrecht, Netherlands : 2001) Netherlands : 2001), 2020-08, Vol.20 (4), p.739-763 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The characteristics of large- and small-scale turbulent motions at roof-level in a street canyon flow were experimentally investigated along with their spatio-temporal organization and their mutual interaction in this region. Quadrant analysis was conducted to identify sweep and ejection events, whilst a spanwise spatial filter was used to identify the large-scale motions in the flow. The present analysis was conducted for six configurations; three upstream roughness arrays and two canyon width (
W
) to height (
h)
aspect ratios (AR =
W/h
= 1 and 3). The upstream roughness arrays consisted of three-dimensional cubes (plan area density,
λ
p
= 25%), 1
h
spaced two-dimensional bars (
λ
p
= 50%, corresponding to the skimming-flow regime) and 3
h
spaced two-dimensional bars (
λ
p
= 25%, corresponding to the wake-interference flow regime). It was found that the roughness configuration has a strong effect on the size of the quadrant events in the street canyon, with the wake-interference flow regimes producing significantly larger sweep and ejection events than the skimming-flow regimes. Upstream wake-interference flow regimes were found to have a significantly greater temporal correlation than in the skimming-flow regimes. Large-scale streamwise and spanwise velocity components were found to have large spatio-temporal correlation integral scales, in agreement with the large-scale structures existing in the overlying boundary layer. It was also confirmed that there is a coupling between large- and small-scales at roof-level of the street canyon. While sweep and ejection events were found to be due to the dynamical contribution of the small-scales, their occurrence is shown to be coupled with that of large-scale low- and high-momentum regions, respectively. |
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ISSN: | 1567-7419 1573-1510 |
DOI: | 10.1007/s10652-019-09721-w |