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Long-term impact of rapid urbanization on urban climate and human thermal comfort in hot-arid environment

机译:快速城市化对热干旱环境中城市气候和人类热舒适的长期影响

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The long-term impact of rapid urbanization on air temperature (Ta), relative humidity (RH), vapor pressure (VP) and human thermal comfort in the Cairo governorate of Egypt was analyzed. Land use change (LUC) between 1973 and 2017 were derived from Landsat satellite data. Next, non-parametric change point and trend detection algorithms were applied to Ta, RH and VP over 1950–2017 to estimate the impacts of urbanization on urban climate. Three historical thermal comfort indices: temperature humidity index (THI), effective temperature index (ETI) and relative strain index (RSI) were estimated from climate data collected between 1950 and 2017 to assess the impact of urbanization on human thermal comfort. The results reveal substantial LUC, rapid increasing impervious surface areas in low-lying areas of Cairo at 75.2 km2/decade since the 1990s. Rapid urbanization had resulted in a statistically significant change point in Taafter 1995 with a warming trend of 0.19 °C/decade, a negative trend in RH of 0.55%/decade and a rising trend in VP of 0.24 hPa/decade. Severe heat stress levels emerged and persisted every July–September since 1994. THI, ETI, and RSI show statistically significant change points at 1994 and a rising trend of 0.33 °C/decade, 0.29 °C/decade, and 0.06/decade, respectively. The highest thermal discomfort risk was found in urban areas of the old Cairo, but the risk is marginally smaller at new cities where there are vegetation covers. This study clearly demonstrates the impacts of rapid urbanization on the urban climate of hot-arid environment.
机译:分析了快速城市化对埃及开罗省的气温(Ta),相对湿度(RH),蒸气压(VP)和人类热舒适度的长期影响。 1973年至2017年之间的土地利用变化(LUC)来自Landsat卫星数据。接下来,在1950-2017年间将非参数变化点和趋势检测算法应用于Ta,RH和VP,以估算城市化对城市气候的影响。根据1950年至2017年收集的气候数据估算了三个历史热舒适指数:温度湿度指数(THI),有效温度指数(ETI)和相对应变指数(RSI),以评估城市化对人类热舒适性的影响。结果表明,自1990年代以来,开罗低洼地区的LUC迅速增加,不透水表面积迅速增加,为75.2平方公里/十年。快速的城市化在1995年以后的Taafter中产生了统计上显着的变化点,变暖趋势为0.19 C /十年,相对湿度为负趋势0.55%/十年,而VP上升趋势为0.24 hPa /十年。自1994年以来,每年的7月至9月出现并持续存在严重的热应力水平。THI,ETI和RSI在1994年显示出统计学上的显着变化点,并且分别上升了0.33°C /十年,0.29°C /十年和0.06 /十年。 。在旧开罗的市区中发现最高的热不适风险,但在植被覆盖的新城市中,该风险略小。这项研究清楚地表明了快速城市化对热干旱环境中城市气候的影响。

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