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eTheses Repository - University of Birmingham

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ort<br />

where U is the wind component orthogonal to the street direction at level IU and<br />

IU<br />

the constant drag coefficient Cd<br />

is set to 0.4, as explained in Martilli et al. (2002).<br />

• The impact <strong>of</strong> the surface is taken into account in the shear and buoyant production<br />

terms in the TKE equation. The extra source term for TKE is due to the fact that the<br />

presence <strong>of</strong> buildings increases the conversion <strong>of</strong> mean kinetic energy into TKE:<br />

Fe<br />

r<br />

3<br />

V<br />

ort V<br />

IU = Cd<br />

U IU S IU<br />

(Equation 3.11)<br />

• Modification <strong>of</strong> the turbulent length scales used to calculate the dissipation term in<br />

the TKE equation. This modification is needed because the presence <strong>of</strong> the<br />

buildings generated vortices which have the same scale as the buildings. The<br />

modification is equivalent to adding a second dissipation terms linked to the scale<br />

<strong>of</strong> the buildings, which has the net effect <strong>of</strong> increasing the dissipation rate and the<br />

cascade <strong>of</strong> mean kinetic energy to TKE.<br />

3.2.2 Calculation <strong>of</strong> thermodynamic effects<br />

The following thermodynamic effects are calculated:<br />

• The turbulent fluxes <strong>of</strong> sensible heat from horizontal surfaces (ro<strong>of</strong>s and canyon<br />

floors) are calculated, as done for the momentum fluxes, using MOST, where fh is<br />

from Louis (1979):<br />

70

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