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Development of a 3-D urbanization index using digital terrain models for surface urban heat island effects

机译:使用数字地形模型开发地表城市热岛效应的3-D城市化指数

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This study assesses surface urban heat island (SUHI) effects during heat waves in subtropical areas. Two cities in northern Taiwan, Taipei metropolis and its adjacent medium-sized city, Yilan, were selected for this empirical study. Daytime and night time surface temperature and SUHI intensity of both cities in five heat wave cases were obtained from MODIS Land-Surface Temperature (LST) and compared. In order to assess SUHI in finer spatial scale, an innovated three-dimensional Urbanization Index (3DUI) with a 5-m spatial resolution was developed to quantify urbanization from a 3-D perspective using Digital Terrain Models (DTMs). The correlation between 3DUI and surface temperatures were also assessed. The results obtained showed that the highest SUHI intensity in daytime was 10.2 ℃ in Taipei and 7.5 ℃ in Yilan. The SUHI intensity was also higher than that in non-heat-wave days (about 5 ℃) in Taipei. The difference in SUHI intensity of both cities could be as small as only 1.0 ℃, suggesting that SUHI intensity was enhanced in both large and medium-sized cities during heat waves. Moreover, the surface temperatures of rural areas in Taipei and Yilan were elevated in the intense heat wave cases, suggesting that the SUHI may reach a plateau when the heat waves get stronger and last longer. In addition, the correlation coefficient between 3DUI and surface temperature was greater than 0.6. The innovative 3DUI can be employed to assess the spatial variation of temperatures and SUHI intensity in much finer spatial resolutions than measurements obtained from remote sensing and weather stations. In summary, the empirical results demonstrated intensified SUHI in large and medium-sized cities in subtropical areas during heat waves which could result in heat stress risks of residents. The innovative 3DUI can be employed to identify vulnerable areas in fine spatial resolutions for formulation of heat wave adaptation strategies.
机译:这项研究评估了亚热带地区热浪期间城市地表热岛(SUHI)的影响。这项经验研究选择了台湾北部的两个城市台北都会及其邻近的中型城市宜兰。从MODIS陆面温度(LST)获得了五个热浪案例中两个城市的白天和晚上的地表温度和SUHI强度,并进行了比较。为了在更精细的空间规模上评估SUHI,开发了一种创新的具有5 m空间分辨率的三维城市化指数(3DUI),以使用数字地形模型(DTM)从3-D角度对城市化进行量化。还评估了3DUI与表面温度之间的相关性。结果表明,白天的最高SUHI强度在台北为10.2℃,在宜兰为7.5℃。台北的SUHI强度也高于非热浪日(约5℃)。两个城市的SUHI强度差异可能只有1.0℃,这表明在大浪中,大中型城市的SUHI强度都增加了。此外,在强烈的热浪情况下,台北和宜兰农村的地表温度升高,这表明当热浪变强且持续时间较长时,SUHI可能达到高原。另外,3DUI与表面温度之间的相关系数大于0.6。与从遥感和气象站获得的测量结果相比,创新的3DUI可用于以更精细的空间分辨率评估温度和SUHI强度的空间变化。总之,实证结果表明,亚热带地区的大中型城市在热浪期间的SUHI加剧,这可能导致居民遭受热应激的风险。创新的3DUI可以用于识别精细空间分辨率中的脆弱区域,从而制定热波适应策略。

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