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

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Similarly, Simmons et al. [41] found that small rain events <strong>of</strong> < 10 mm were all retained inthe green ro<strong>of</strong>s. For rain event <strong>of</strong> 12 mm the retention between the green ro<strong>of</strong>s varied from 88% to 26 % depending on the substrate <strong><strong>an</strong>d</strong> drainage type. <strong>The</strong> rain events <strong>of</strong> 28 mm <strong><strong>an</strong>d</strong> 49mm showed a retention <strong>of</strong> 8 - 43 % <strong><strong>an</strong>d</strong> 13 – 44 % respectively. It was further observed thatthe retention depends upon the rain event intensity ch<strong>an</strong>ges as well as the rain event size.6.22 Role <strong>of</strong> VegetationMost studies show that the type <strong><strong>an</strong>d</strong> depth <strong>of</strong> substrate has the major influence on green ro<strong>of</strong>water capacity <strong><strong>an</strong>d</strong> not the vegetation type.However, the type <strong><strong>an</strong>d</strong> cover <strong>of</strong> vegetation does play a role in the water retention <strong><strong>an</strong>d</strong> run<strong>of</strong>fcharacteristics <strong>of</strong> a green ro<strong>of</strong>. This is mainly during summer months, when there is lowerwater availability <strong><strong>an</strong>d</strong> higher temperatures.6.23 Influence <strong>of</strong> Slope<strong>The</strong> influence <strong>of</strong> slope on the run<strong>of</strong>f <strong><strong>an</strong>d</strong> retenetion characteristics <strong>of</strong> green ro<strong>of</strong>s variesbetween studies. Some studies such as Bengtsson [42] find no correlation between ro<strong>of</strong> slope<strong><strong>an</strong>d</strong> run<strong>of</strong>f, whereas a study by Getter et al. [43] found that run<strong>of</strong>f retention may depend uponthe slope.<strong>The</strong> effect <strong>of</strong> the ro<strong>of</strong> slope combines with other factors such as the substrate properties,intensity <strong>of</strong> rainfall event, flow conditions, the design <strong><strong>an</strong>d</strong> type <strong>of</strong> green ro<strong>of</strong> layers(especially drainage).<strong>The</strong> study mentioned by Getter et al. [43] found that for different rainfall events (light < 2mm, medium 2 – 10 mm, heavy > 10 mm) both the type <strong>of</strong> rainfall event <strong><strong>an</strong>d</strong> slope hadsignific<strong>an</strong>t influence over water retention. Water retention for the lowest gradient <strong>of</strong> slopewas 85 %, whereas for higher gradients 75 % <strong>of</strong> precipitation was retained (as <strong>an</strong> average <strong>of</strong>results). It was also found that retention was higher for light rain events (94 %) th<strong>an</strong> for heavyrain events (63 %) - as would be expected.Niall Carroll Page 43<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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