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Fraction <strong>of</strong> urban land cover [%]<br />

Figure 5.2: Percentage <strong>of</strong> urban land use in the domain (taken from the CEH Land Cover<br />

2000 data).<br />

The simulations were 48-72 hours long, depending on the cases. Periods were chosen with<br />

anti-cyclonic meteorological conditions characterised by relatively clear skies and low<br />

winds, since these are found to be favourable to the development <strong>of</strong> a strong UHI (GLA<br />

2006). In particular the heat island is found to be small when cloud cover exceeds 4 oktas,<br />

although cloud cover alone cannot be used as a predictor <strong>of</strong> strong heat island events (GLA<br />

2006). This allows the cloud and rain parameterisation schemes in the METRAS model to<br />

be switched <strong>of</strong>f, saving computational time.<br />

In order to select simulation periods characterised by these conditions, the Lamb Weather<br />

classification (Hulme et al. 1997) was obtained for each day for the summer (June, July and<br />

August - JJA) and winter months (December, January and February - DJF) <strong>of</strong> years 1995-<br />

2000. The Lamb classification is based on surface synoptic charts, which represent the state<br />

<strong>of</strong> the atmospheric circulation close to the ground, and charts at the 500 hPa level. There<br />

are three non-directional types, anti-cyclonic (A), cyclonic (C), which are dependent on<br />

135

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