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Urban Heat Island Mitigation Effectiveness under Extreme Heat Conditions in the Suzhou-Wuxi-Changzhou Metropolitan Area, China

机译:苏州 - 无锡常州大都市地区极端散热下的城市热岛缓解效率

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摘要

Cool roofs and green roofs are two important methods used to mitigate the urban heat island (UHI) effect. The Weather Research and Forecasting Model was used to investigate the UHI effect and the effectiveness of cool and green roof mitigation strategies in the Suzhou-Wuxi-Changzhou metropolitan area during an extreme heat wave episode in the summer of 2013. Both urban land-cover change and anthropogenic heat releases exacerbated high temperatures in the urban area. Notably, urban land-cover change and anthropogenic heat release were responsible for 64% and 36% of the UHI intensity, respectively. Both cool and green roofs decreased near-surface air temperatures. The most dramatic decrease in near-surface air temperature occurred in the late morning; nocturnal air temperature decreased slightly because of the decrease in urban heat storage associated with the cool roof strategy. In addition, the UHI mitigation strategies affected the entire urban boundary layer. The decrease in the potential temperature and static stability created a stable urban boundary layer in which turbulent kinetic energy (TKE) decreased simultaneously. Analysis of an urban belt near a large water body showed that the decrease in the surface skin temperature difference between land and the water body weakened the daytime lake breeze. This effect was observed in both the inflow in the boundary layer and the return flow above the boundary layer, and it decreased the heat and moisture exchange between the lake and land boundary layers.
机译:凉爽的屋顶和绿色屋顶是用于减轻城市热岛(UHI)效应的两个重要方法。天气研究和预测模型用于探讨苏州 - 无锡常州大都市区在2013年夏季苏州 - 无锡常州大都市区舒通效应及其有效性。城市土地覆盖变革和人为热释放在市区加剧了高温。值得注意的是,城市陆地覆盖变化和人为热释放分别负责64%和36%的UHI强度。凉爽和绿色屋顶均降低了近表面空气温度。最急剧下降的近天的气温下降;由于与凉爽的屋顶策略相关的城市蓄热量减少,夜间空气温度略有下降。此外,UHI缓解策略影响了整个城市边界层。潜在温度和静态稳定性的降低产生了一种稳定的城市边界层,湍流动能(TKE)同时降低。大型水体附近的城市带分析表明,陆地和水体之间的表面肌肤温差降低削弱了白天湖风。在边界层中的流入和边界层上方的返回流程中观察到这种效果,并且它降低了湖泊和陆边界层之间的热量和水分交换。

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