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Wind-driven rain and future risk to built heritage in the United Kingdom: Novel metrics for characterising rain spells

机译:风雨和英国建筑遗产的未来风险:表征雨季的新指标

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Wind-driven rain (WDR) is rain given a horizontal velocity component by wind and falling obliquely. It is a prominent environmental risk to built heritage, as it contributes to the damage of porous building materials and building element failure. While predicted climate trends are well-established, how they will specifically manifest in future WDR is uncertain. This paper combines UKCP09 Weather Generator predictions with a probabilistic process to create hourly time series of climate parameters under a high-emissions scenario for 2070–2099 at eight UK sites. Exposure to WDR at these sites for baseline and future periods is calculated from semi-empirical models based on long-term hourly meteorological data using ISO 15927-3:2009. Towards the end of the twenty-first century, it is predicted that rain spells will have higher volumes, i.e. a higher quantity of water will impact façades, across all 8 sites. Although the average number of spells is predicted to remain constant, they will be shorter with longer of periods of time between them and more intense with wind-driven rain occurring for a greater proportion of hours within them. It is likely that in this scenario building element failure – such as moisture ingress through cracks and gutter over-spill – will occur more frequently. There will be higher rates of moisture cycling and enhanced deep-seated wetting. These predicted changes require new metrics for wind-driven rain to be developed, so that future impacts can be managed effectively and efficiently.
机译:风雨(WDR)是指由于风而产生的水平速度分量并倾斜下降的雨。对于建筑遗产而言,这是一个突出的环境风险,因为它会导致多孔建筑材料的损坏和建筑构件的破坏。尽管预测的气候趋势已经确立,但在未来的WDR中将如何具体体现尚不确定。本文将UKCP09天气生成器的预测与一个概率过程结合起来,以在英国八个站点的2070-2099年高排放情景下,创建气候参数的每小时时间序列。根据ISO 15927-3:2009的长期小时气象数据,通过半经验模型计算出这些地点在基线和未来时期的WDR暴露。预计到21世纪末,所有8个地点的雨水量将增加,即,大量的水将影响立面。尽管预计平均咒语数量将保持不变,但它们之间的时间间隔越短,它们就会越短,而在更大范围的小时数内,随风而下的降雨会加剧这种情况。在这种情况下,建筑元件故障(例如,通过裂缝渗入水分和排水沟过度溢出)可能会更频繁地发生。水分循环的速率会更高,深层润湿性也会增强。这些预测的变化需要开发用于风雨的新指标,以便可以有效地管理未来的影响。

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