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ASI2_Lecture 3_7/12/2011<br />

Potential exposure assessment application:<br />

Theory- Pollution retention in urban canyons<br />

Courtesy <strong>of</strong> J. Richmond-Bryant<br />

U<br />

U<br />

WIND<br />

D<br />

l<br />

WIND<br />

D<br />

W<br />

• H = Uτ/D = f(UD/ν, k 0.5 /U, l/D, D/W)<br />

= f(Re, turbulence intensity, shape)<br />

o H = nondimensional residence time <strong>of</strong> pollutant in canyon<br />

o τ = residence time<br />

o k = turbulence kinetic energy <strong>of</strong> the wind<br />

o ν = kinematic viscosity<br />

o Re = Reynolds number<br />

• Based on dimensional analysis and derived from the equation<br />

<strong>of</strong> scalar flux transport (Humphries & Vincent 1976)<br />

ASI 2: URBAN CLIMATE AND AIR POLLUTION <strong>School</strong> <strong>of</strong> <strong>Architecture</strong>, The Chinese University <strong>of</strong> Hong Kong, Hong Kong, 7-8 Dec 2011<br />

Residence time H vs D/W<br />

Courtesy <strong>of</strong> J. Richmond-Bryant<br />

Mid Manhattan05<br />

• Significant fit:<br />

o H = 22(D/W) -0.69<br />

o R 2 = 0.62<br />

o p < 0.001<br />

Two Cities MM and<br />

OkCity<br />

• Poor fit:<br />

o H = 51(D/W) -0.812<br />

o R 2 = 0.035<br />

o p = 0.022<br />

JU2003: OklCity<br />

• Scatter visible<br />

• Novel methodology, under development<br />

• Significant fit:<br />

• Qualitatively similar results for two<br />

o H = 296(D/W) cities<br />

-0.812<br />

o R 2 = 0.48<br />

• Two cities differ quantitatively<br />

o p < 0.0001<br />

• Parameterizations can utilize fine scale<br />

modeling to provide inputs for exposure<br />

assessment<br />

• Improved methodologies with multiple<br />

canopy formulation sets such as from<br />

ASI 2: URBAN CLIMATE AND AIR POLLUTION NUDAPT to be tested.<br />

<strong>School</strong> <strong>of</strong> <strong>Architecture</strong>, The Chinese University <strong>of</strong> Hong Kong, Hong Kong, 7-8 Dec 2011<br />

16

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