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eTheses Repository - University of Birmingham

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2.5 Summary<br />

This review has considered the urban modifications to the mechanical, thermal and<br />

hydrological properties <strong>of</strong> the atmosphere. It is difficult to make representative<br />

measurements <strong>of</strong> urban modifications, and to represent all the effects <strong>of</strong> the urban surface<br />

in a model. Modelling studies are however a useful way <strong>of</strong> investigating effects <strong>of</strong> the<br />

urban surface that can not be easily measured at representative scales and <strong>of</strong> providing<br />

information regarding the impact <strong>of</strong> past and future examples <strong>of</strong> urban land cover.<br />

Mesoscale modelling studies on the effects <strong>of</strong> urbanisation to date are limited, and few<br />

studies exist which use a sophisticated parameterisation <strong>of</strong> the urban surface to simulate<br />

urban effects.<br />

Possible ways <strong>of</strong> representing the urban surface in mesoscale models are reviewed. In order<br />

to address the aims <strong>of</strong> this study <strong>of</strong> understanding how changes in land cover due to<br />

urbanisation have affected the London region, a multi-layer urban canopy scheme (BEP) is<br />

implemented into the mesoscale model METRAS. This sophisticated treatment <strong>of</strong> the<br />

urban surface, together with that fact that the model is run at a much higher spatial<br />

resolution than past studies (1 km compared to for example 10 km for Trusilova et al.<br />

(2006)) make it possible to investigate the effect <strong>of</strong> urbanisation for a single area in much<br />

greater detail, with input data specific to the city <strong>of</strong> London rather than representative <strong>of</strong> all<br />

European cities, and past and future urbanisation scenarios, as well as a base line with no<br />

urban areas, specific to London. As for many past studies, the focus will be on<br />

representative cases <strong>of</strong> anti-cyclonic conditions which are favourable to the development <strong>of</strong><br />

urban effects such as the urban heat island, rather than long term model runs which are<br />

computationally very expensive and which, when average monthly or seasonally, smooth<br />

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