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BPS5234A Chap.11 Street Canyons and Urban Morphology

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Chapter 11 of 12 · BPS5234A

Street Canyons and Urban Morphology

Geometry decides ventilation

The street canyon lab holds the street width at 20 m and raises the buildings from 10 to 20 to 40 m, giving height-to-width ratios of 0.5, 1.0 and 2.0. With the wind perpendicular to the street, the shallow canyon behaves as isolated roughness, the square canyon holds a single vortex in wake interference, and the deep canyon shows skimming flow, with a shear layer at roof level over a trapped vortex and possibly a weaker secondary vortex beneath.

Ventilation and pollutant removal worsen in that order.

Setting up the canyon

The canyon is run in two dimensions with a steady RNG k–&epsilon model, enhanced wall treatment, a 3 m/s inlet and a T-shaped domain after a published study. Refinement at roof edges, ground and walls with ten inflation layers and a target y+ of 1 to 30 decides whether the shear layer and vortex are captured.

The deliverables are plots of speed, streamlines and vorticity together with vertical velocity profiles.

Four urban forms

The morphology lab compares open, medium-density, dense and mixed-height block layouts with an atmospheric inlet at 3 m/s, rough ground and a realizable k–&epsilon model.

Open layouts ventilate well; medium layouts show recirculation and channelling; dense layouts stagnate; mixed-height layouts mix strongly through downwash. The course follow-up limits the exercise to nine buildings, four layouts and one wind direction.

Reading amplification

The velocity amplification factor divides pedestrian-level speed by the reference speed.

Dense layouts show both very low and very high values in the same district.

In this chapter

What this chapter covers

  • 01

    Canyon aspect ratio and the three flow regimes

  • 02

    Shear layer, main vortex and secondary vortex

  • 03

    Canyon set-up decisions and vortex diagnostics

  • 04

    Open, medium, dense and mixed-height layouts

  • 05

    The velocity amplification factor at pedestrian height

  • 06

    Design levers for high and low amplification

Worked example · free

Placing a real street on the regime scale

Q [5 marks]. A city street is 12 m wide between continuous blocks 36 m tall. A second street is 30 m wide between blocks 15 m tall. Compute each aspect ratio, place each against the lab’s three cases, and rank them for clearing traffic pollutant with perpendicular wind. The step weighting shown here is an AskSia study allocation and is not a University marking scheme.
Figure 11.1.Figure 11.1. The three canyons of the lab. As the ratio rises the wind stops entering the street and skims over a trapped vortex; the deepest case can hold a second, weaker vortex below.H/W = 0.5isolated roughnessH/W = 1.0wake interferenceH/W = 2.0skimming flowshear layer
Figure 11.1. The three canyons of the lab. As the ratio rises the wind stops entering the street and skims over a trapped vortex; the deepest case can hold a second, weaker vortex below.
  • 2Compute the height-to-width ratio of each street.
  • 2Place each against the lab cases and their regimes.
  • 1Rank them for pollutant removal with a reason.
The first street has H/W = 36 / 12 = 3.0, deeper than the lab’s deepest case of 2.0, so skimming flow with weak exchange is expected and a secondary vortex is plausible near the floor. The second has H/W = 15 / 30 = 0.5, matching the lab’s shallow case of isolated roughness flow, where the wind reaches the street and exchanges strongly with the air above. The second street therefore clears pollutant far better. For the deep street, the useful design questions are whether gaps, setbacks or height variation can break the skimming layer, and any simulation of it needs fine resolution at roof level to capture the shear layer.
Sia tip — Compute H/W from the actual building heights on both sides; an uneven canyon behaves differently from the symmetric lab cases, so say so.
Glossary

Key terms

Street Canyon
A street flanked by continuous buildings on both sides, characterised by its height-to-width ratio.
Skimming Flow
The regime in a deep canyon where the wind passes over a roof-level shear layer and drives a trapped vortex below.
Wake Interference Flow
The intermediate regime in which the wake of one building reaches the next and a single vortex fills the canyon.
Building Coverage Ratio
The share of site area covered by building footprints, one of the descriptors of an urban morphology.
Q-Criterion
A field quantity used to identify vortex cores more reliably than velocity magnitude alone.
FAQ

Street Canyons and Urban Morphology FAQ

Why does a deeper canyon ventilate worse?

As the canyon deepens the wind stops descending into it and skims over a shear layer at roof level. The trapped vortex beneath exchanges air with the flow above only weakly, so pollutant released at street level is retained rather than removed.

Why use vorticity or the Q-criterion for canyon results?

Velocity contours can make a weak vortex invisible, especially a secondary vortex low in a deep canyon. Vorticity and the Q-criterion locate vortex cores directly, which is what the lab asks for when it requires the vortex centre to be extracted.

Why does a mixed-height layout often ventilate better than a uniform dense one?

Uneven heights generate extra turbulence and drive air vertically, through downwash and colliding shear layers, so air is brought down into the street even when building coverage is similar. The model answers favour it for tropical cities on that ground, since it also keeps the streets shaded.

What does a velocity amplification factor above 2.0 indicate?

That the pedestrian-level wind is more than twice the reference speed, typically at corners and gaps in dense layouts. The model answers point to four levers for shrinking such areas: a more porous layout, varied heights, wider passages, and podiums that let air pass.

Why scale the morphology domain on the tallest building?

Domain extents set in multiples of the tallest height let the inflow develop and the wakes recover without blockage or artificial effects. Shortening the upstream length from 5H to 2H would distort the inlet turbulence and velocity profiles and so the pedestrian-level speeds.

Study strategy

Assessment move

Draw the three canyon regimes and the four morphologies as thumbnail sketches with arrows, then write one sentence under each about ventilation. Rehearse explaining the change from one sketch to the next, because the tutorial questions ask why the regime changes, not only what it is.

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