Abstract
The urban heat island intensity (difference between a semi-rural and urban dry bulb air temperature, urban heat island intensity) has been analysed for Manchester using data from 1996 to 2011. The semi-rural sites were airfields and the urban site was 2 km from the centre of Manchester. Although the urban site was not as developed as the city centre it showed a significant urban heat island intensity. A stochastic model developed from the data showed that the maximum mean daily value would be about 6℃ which compared well with more detailed measurements. However, there was a highly significant trend of increasing urban heat island intensity which by the end of the century could add 2.4 K to the predicted climate change increase. An analysis of the urban morphology showed that the urban site had indeed become more urban over 9 years of the study, losing green spaces which mitigate against the urban heat island intensity.
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