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Short range dispersion in urban areas Alan Robins, University of - - PowerPoint PPT Presentation
Short range dispersion in urban areas Alan Robins, University of - - PowerPoint PPT Presentation
Short range dispersion in urban areas Alan Robins, University of Surrey DAPPLE team Surrey - wind tunnel modelling, analysis Bristol - tracer studies, analysis Cambridge - tracer studies, modelling & applications Imperial - personal
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From canyons to intersections - early work Some features of dispersion in cities using London as an example Some sensitivity studies Implications for regulatory/emergency response modelling
Content
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Four blocks
Athena Scaperdas
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Four blocks - velocity vectors
Measured Velocity Vectors (LDA) z/H = 0.16, Orientation = 10 degs U/Uref
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Four blocks - exchanges
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Streets and intersections
Where are the classical street canyons? The city as a set of short streets between intersections. Concentrate
- n the
intersections. Use London as an example (of a certain class of cities). AURN Site
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A simple model for generic use
Initial wind tunnel model
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Flow field
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Horizontal mean velocity vectors at heights of 5 and 20 m
Mean flow field at an intersection
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Mean velocity vectors at heights of 5 m
Mean flow field at an intersection
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Mean velocity vectors at heights of 5 m
Mean flow field at an intersection
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Flow visualisation
Flow ‘switching’ with diagonal winds - bimodal pdfs? Light sheet at about z/H = 0.3
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Flow visualisation
Horizontal light sheet near surface Vertical light sheet along centre of road Vertical light sheet along centre of road
Source
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Light sheet along Marylebone Road
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Light sheet along Marylebone Road
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Vertical sheet along Marylebone Rd
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Vertical sheet along Marylebone Rd
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Vertical sheet along Gloucester Pl
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Vertical sheet along Gloucester Pl
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Flow visualisation and LES
- 1. Exchanges through a street
network
- 2. Loss/gain to flow above roof
level.
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Network models - SIRANE
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∫ ∫ ( U C + < u c > ) d A
Flux balances - mean and turbulent
?
U, UT, UN
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SIRANE
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Some empirical results
C* = CU(H)H 2 / Q c'* = c'U(H)H 2 / Q Separation R* = R / H Review C *(R / H), c'*(R / H) Ground level source in a boundary layer C* (R / H)N, N = 1.5 1.8 c'/ C 0.5 0.7
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Mean concentration
C* = 12/R*2 downwind sector only
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Salt Lake City
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Concentration fluctuations
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Fluctuation intensity
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Single events (realisations) may differ greatly from the mean of a large number (ensemble) of repeated events. Field studies provide a collection of realisations … that are not part of a common ensemble.
Receptor position 1- plume edge
ensemble mean in white, realisations in red
Variability amongst realisations
Receptor position 6- plume centre
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Scatter plot for individual releases
1:1 correspondence
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Sensitivity studies
Monitor air quality where?
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Comparison of results from low and higher resolution models; significant differences confined to short ranges.
Model detail
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Comparison of results from low and higher resolution models; significant differences confined to short ranges.
Model detail
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Generic upwind building arrangement
Upwind model detail
Source ‘X’
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Upwind model detail
Concentrations, C*, across the main intersection for source at X, wind direction 51˚
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Upwind model detail
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Reference; blockage at A, B or C; blockage at A, B & C. Green, reference; blue, blockage at A; red, at D; yellow at A & D. Wind direction
- 90, degs
Wind direction
- 45, degs
Blocked streets
Concentrations along Marylebone Road
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Car speed profile during one experiment Roadside sampler locations
Moving source
Not a line source - a set of point sources.
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Moving source
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Decay law C* = 12 R H
- 2
Threshold CL* = 10 RL H
- 2
Contaminated region RL = H 10 CL *
- 1/2
RL RL RL
“Source” street
Empirical modelling
Upwind spread
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Regulatory level modelling
Exchanges at intersections are a fundamental feature Near-classical canyon conditions within about a street width Substantial fluxes above roof level (even at short range) Substantial parameter data base to acquire and test Then add isolated tall buildings, open spaces, etc.
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Advanced level modelling
Relatively weak sensitivity to model detail Generic upwind conditions appear adequate Substantial unsteadiness Intermittent dispersion process important Provision of parameters for regulatory level models
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Some questions
Choice of reference wind Street roughness elements (buses, trees …) Evaluation against field data Unsteady source terms Thermal effects, light winds, traffic
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