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A Comprehensive Statistical Study on Daytime Surface Urban Heat Island during Summer in Urban Areas, Case Study: Cairo and Its New Towns

机译:城市夏季白天地表城市热岛的综合统计研究,以开罗及其新城为例

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Surface urban heat island (SUHI) is defined as the elevated land surface temperature (LST) in urban area in comparison with non-urban areas, and it can influence the energy consumption, comfort and health of urban residents. In this study, the existence of daytime SUHI, in Cairo and its new towns during the summer, is investigated using three different approaches; (1) utilization of pre-urbanization observations as LST references; (2) utilization of rural observations as LST references (urban–rural difference); and (3) utilization of the SIUHI (Surface Intra Urban Heat Island) approach. A time series of Landsat TM & ETM+ data (46 images) from 1984 to 2015 was employed in this study for daytime LST calculation during summer. Different statistical hypothesis tests were utilized for the evaluation of LST and SUHI in the case studies. The results demonstrated that there is no significant LST difference between the urban areas studied, and their corresponding built-up areas. In addition, daytime LST in new towns during the summer is 2 K warmer than in Cairo. Utilization of a pre-urbanization observations approach, alongside an evaluation of the long-term trend, demonstrated that there is no daytime SUHI during the summer in the study areas, and construction activities in the study areas do not result in cooling or warming effects. Utilization of the rural observations approach showed that LST is lower in Cairo than its surrounding areas. This demonstrates why the selection of suitable rural references in SUHI studies is an important and complicated task, and how this approach may lead to misinterpretation in desert city areas with significant landscape and surface difference with their most surrounding areas (e.g., Cairo). Results showed that, although SIUHI technique can be representative for the changes of variance of LST in urban areas, it is not able to identify the changes of mean LST in urban areas.
机译:地表城市热岛(SUHI)被定义为城市地区与非城市地区相比升高的地表温度(LST),它会影响城市居民的能源消耗,舒适度和健康状况。在这项研究中,使用三种不同的方法调查了夏季开罗及其新市镇白天SUHI的存在。 (1)利用城市化前的观测作为LST参考; (2)利用农村观测作为LST参考(城乡差异); (3)利用SIUHI(城市内部城市热岛)方法。这项研究使用1984年至2015年的Landsat TM和ETM +数据的时间序列(46张图像)进行夏季的白天LST计算。在案例研究中,使用了不同的统计假设检验来评估LST和SUHI。结果表明,在研究的城市区域及其相应的建成区之间,LST没有显着差异。此外,夏季新市镇的白天LST比开罗高2K。利用城市化前的观察方法,以及对长期趋势的评估,表明研究区域夏天没有白天的SUHI,并且研究区域的建筑活动不会导致降温或变暖的影响。利用农村观察方法表明,开罗的LST低于其周围地区。这说明了为什么在SUHI研究中选择合适的农村参考文献是一项重要而复杂的任务,以及这种方法如何可能导致在沙漠城市地区及其周边地区(例如开罗)具有明显的景观和地表差异的错误解释。结果表明,尽管SIUHI技术可以代表城市地区LST方差的变化,但它无法识别城市地区平均LST的变化。

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