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eTheses Repository - University of Birmingham

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8.2 Improvements and recommendations for future work<br />

The work in this PhD study, and in particular the scenarios for past and future urbanisation<br />

presented in Chapters 6 and 7, has been limited by the computational demand <strong>of</strong> the<br />

METRAS+BEP model and the resources available at the <strong>University</strong> <strong>of</strong> <strong>Birmingham</strong>. A<br />

valuable recommendation for future work would be to devise a faster implementation <strong>of</strong> the<br />

urban module within METRAS and the use <strong>of</strong> the parallelised version <strong>of</strong> the model<br />

METRAS. Longer simulations would allow a better assessment <strong>of</strong> the urban effects <strong>of</strong><br />

climate, for example following some <strong>of</strong> the methods in Lamptey et al. (2005) and Trusilova<br />

et al. (2008) to do a statistical analysis <strong>of</strong> the effects <strong>of</strong> the urban surface.<br />

Due to the computational demand <strong>of</strong> the modelling system, the scope <strong>of</strong> the analysis has<br />

been strictly limited to near surface impacts on temperature and wind speed in and around<br />

the urban area. Future work could extend this scope, for example considering the effects <strong>of</strong><br />

the urbanisation land cover change on the boundary layer structure, surface energy balance.<br />

An extension <strong>of</strong> the model to include air chemistry would permit the model meteorological<br />

results to be linked to air quality studies in the urban area.<br />

This PhD study has focussed on the simulation <strong>of</strong> cloud and rain free days in order to<br />

reduce complexity and computational demand. The inclusion <strong>of</strong> these subroutines could<br />

permit an investigation into the effects <strong>of</strong> the urban area on precipitation. Numerical studies<br />

<strong>of</strong> this sort have been undertaken for many urban areas (Thielen et al. 2000; e.g. Trusilova<br />

2006; Lin et al. 2008) and some experimental studies have observed that the London urban<br />

heat island can trigger storms (Atkinson 1968; Hand et al. 2004).<br />

240

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