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eTheses Repository - University of Birmingham

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appropriate value for these parameters to use in future work on the city <strong>of</strong> London is not<br />

easy, and there is little available literature to assist in the choice.<br />

Potential temperature [K]<br />

Figure 4.16: Potential temperature (K) along the line y=0, z=10 m, as computed by the three<br />

simulations with the internal temperatures behind urban walls and ro<strong>of</strong>s (‘twini’ and ‘trini’) both set to<br />

293 K (black line), 295 K (green) and 297 K (yellow) at 04:00 for the second day <strong>of</strong> simulation.<br />

4.3.3 Sensitivity to the surface albedo<br />

The sensitivity <strong>of</strong> the model to the albedo values <strong>of</strong> the urban surfaces was investigated.<br />

The albedo <strong>of</strong> a surface is defined as its hemispherically and wavelength integrated<br />

reflectivity (Taha 1997).<br />

The difference in albedo between rural and urban surfaces is one <strong>of</strong> the factors which can<br />

affect the surface energy balance in urban areas. The albedo for the urban area is typically<br />

lower than that <strong>of</strong> the rural surroundings, and therefore less radiation is reflected back from<br />

the urban area, which can lead to a higher heat content, thus contributing to the UHI<br />

phenomenon (Oke 1987; Taha 1997; Atkinson 2003). A decrease in the UHI intensity is<br />

111

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