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Coupled Pavement-Urban Canyon Model for Assessing Cool Pavements

机译:评估凉爽路面的人行道-城市峡谷耦合模型

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One of the primary causes of the urban heat island (UHI) effect is the use of construction materials that absorb and store more heat than natural vegetation. Additional heating and temperature rise occurs because of the coupling between man-made surfaces and the air in urban areas. A coupled pavement-urban canyon model has been developed and applied to a hypothetical urban domain with 12 urban canyons in order to quantify the microscale UHI intensity for the statistically warmest hour of the year in Chicago, USA. The control pavement with low albedo and diffusivity had a microscale UHI intensity of 4.2—5.1°C as compared to the mesoscale intensity of 4°C. When the control pavement was replaced by a cool pavement of higher albedo and diffusivity, the microscale UHI intensity decreased in all the canyons to 4.0— 4.4°C as compared to the control. The decrease in UHI magnitude ranged from 0.1-0.7°C with an average decrease of 0.4°C.
机译:城市热岛效应(UHI)的主要原因之一是使用比自然植被吸收和储存更多热量的建筑材料。由于人造表面与城市区域中的空气之间的耦合,因此会产生额外的热量和温度升高。已经开发了人行道-城市峡谷耦合模型,并将其应用于具有12个城市峡谷的假设城市领域,以便量化美国芝加哥一年中统计上最温暖的小时的微尺度UHI强度。与4°C的中尺度强度相比,具有低反照率和扩散率的对照路面的UHI微观尺度强度为4.2-5.1°C。当用高反照率和扩散率的凉爽路面代替对照路面时,与对照相比,所有峡谷的微尺度UHI强度均降低至4.0- 4.4°C。 UHI幅度的下降范围为0.1-0.7°C,平均下降幅度为0.4°C。

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