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The Thermal and Rainwater Runoff Performance of an Extensive ...

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<strong>The</strong> urb<strong>an</strong> heat isl<strong><strong>an</strong>d</strong> effect describes the phenomena <strong>of</strong> higher average temperatures inurb<strong>an</strong> areas compared with surrounding rural areas. This c<strong>an</strong> lead to <strong>an</strong> increase in air-bornpollution <strong><strong>an</strong>d</strong> <strong>an</strong> increased use <strong>of</strong> air conditioning.Figure 14: Example <strong>of</strong> Urb<strong>an</strong> Heat Isl<strong><strong>an</strong>d</strong> Effect [18]A number <strong>of</strong> complex factors contribute to the urb<strong>an</strong> heat isl<strong><strong>an</strong>d</strong> effect. <strong>The</strong>se include [19]:• Reduction <strong>of</strong> evaporating surfaces – more energy turned into sensible heat <strong><strong>an</strong>d</strong>less into latent heat• <strong>The</strong>rmal properties <strong>of</strong> materials – increased storage <strong>of</strong> sensible heat in buildingfabric• Anthropogenic heat released – from combustion <strong>of</strong> fuels <strong><strong>an</strong>d</strong> metabolism <strong>of</strong><strong>an</strong>imals/people• C<strong>an</strong>yon radiative effect – decrease <strong>of</strong> long-wave radiation lost to the sky <strong><strong>an</strong>d</strong>retained in the urb<strong>an</strong> area due to radiation interch<strong>an</strong>ge between especially tallbuildings within relatively narrow streets <strong><strong>an</strong>d</strong> reduction <strong>of</strong> albedo due to multiplereflection <strong>of</strong> short-wave radiation between building surfacesNiall Carroll Page 33<strong>The</strong> <strong>The</strong>rmal <strong><strong>an</strong>d</strong> <strong>Rainwater</strong> <strong>Run<strong>of</strong>f</strong> <strong>Perform<strong>an</strong>ce</strong> <strong>of</strong> <strong>an</strong> <strong>Extensive</strong> Green Ro<strong>of</strong> System

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