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eTheses Repository - University of Birmingham

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educed near surface temperatures <strong>of</strong> more than 1 K. Moreover these temperature changes<br />

were not always confined to the grid cells for which the land cover classification had been<br />

modified. Dhakal et al. (2002) found the maximum reduction in average noon temperatures<br />

due to greening the area surrounding the buildings to be 0.47 K. Another benefit <strong>of</strong> urban<br />

vegetation, and especially <strong>of</strong> trees, is the effect on air quality. For example Nowak et al.<br />

(2000) showed that increased tree cover can help reduce high ozone concentrations and<br />

those <strong>of</strong> other pollutants. Simulations in Taha (1996) indicated that the net effect <strong>of</strong><br />

increased urban vegetation was a decrease in ozone concentrations, if the trees are low<br />

emitters.<br />

In the control simulation the urban area had no vegetated fraction at all. This is obviously<br />

not a very realistic situation, although some Mediterranean cities have a very low fraction<br />

<strong>of</strong> vegetation, but the choice was made in order to ease the interpretation <strong>of</strong> the model<br />

results for the test case. Two further simulations were carried out:<br />

• veg1: 10% vegetation evenly distributed within the urban area<br />

• veg2: 30% vegetation evenly distributed within the urban area<br />

In particular, 30% is a realistic assumption for the vegetated fraction and is a good<br />

approximation for the city <strong>of</strong> London, where the vegetation coverage is estimated at 20-<br />

30% (www.english-heritage.org.uk). The vegetated area was treated as the METRAS land<br />

cover class <strong>of</strong> ‘Meadows’, the rest <strong>of</strong> the urban area was treated with the BEP urban<br />

scheme.<br />

117

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