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首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Monitoring surface urban heat island formation in a tropical mountain city using Landsat data (1987-2015)
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Monitoring surface urban heat island formation in a tropical mountain city using Landsat data (1987-2015)

机译:使用Landsat数据监控热带山区城市的地表城市热岛形成(1987-2015)

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Since it was first described about two centuries ago and due to its adverse impacts on urban ecological environment and the overall livability of cities, the urban heat island (UHI) phenomenon has been, and still is, an important research topic across various fields of study. However, UHI studies on cities in mountain regions are still lacking. This study aims to contribute to this endeavor by monitoring and examining the formation of surface UHI (SUHI) in a tropical mountain city of Southeast Asia-Baguio City, the summer capital of the Philippines- using Landsat data (1987-2015). Based on mean surface temperature difference between impervious surface (IS) and green space (GS1), SUHI intensity (SUHII) in the study area increased from 2.7 degrees C in 1987 to 3.4 degrees C in 2015. Between an urban zone (>86% impervious) and a rural zone (<10% impervious) along the urban-rural gradient, it increased from 4.0 degrees C in 1987 to 8.2 degrees C in 2015. These results are consistent with the rapid urbanization of the area over the same period, which resulted in a rapid expansion of impervious surfaces and substantial loss of green spaces. Together with landscape composition variables (e.g. fraction of IS), topographic variables (e.g. hillshade) can help explain a significant amount of spatial variations in surface temperature in the area (R-2 = 0.56-0.85) (p < 0.001). The relative importance of the 'fraction of IS' variable also increased, indicating that its unique explanatory and predictive power concerning the spatial variations of surface temperature increases as the city size becomes bigger and SUHI gets more intense. Overall, these results indicate that the cool temperature of the study area being situated in a mountain region did not hinder the formation of SUHI. Thus, the formation and effects of UHIs, including possible mitigation and adaptation measures, should be considered in landscape planning for the sustainable urban development of the area. (C) 2017 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
机译:自从大约两个世纪前首次对其进行描述以来,由于其对城市生态环境和城市总体宜居性的不利影响,城市热岛(UHI)现象一直是而且仍然是各个研究领域的重要研究课题。 。但是,仍然缺乏关于山区城市的UHI研究。这项研究旨在通过使用Landsat数据(1987-2015年)监测和检查东南亚热带山区城市碧瑶市(菲律宾夏季首都碧瑶市)中地表超高热(SUHI)的形成,从而为这一工作做出贡献。根据不透水表面(IS)与绿地(GS1)之间的平均表面温差,研究区域的SUHI强度(SUHII)从1987年的2.7摄氏度增加到2015年的3.4摄氏度。在城市地区(> 86%)不透水)和沿城乡梯度变化的农村地区(<10%不透水),从1987年的4.0摄氏度增加到2015年的8.2摄氏度。这些结果与同期该地区的快速城市化是一致的,导致不透水表面的迅速膨胀和绿色空间的大量损失。与地形组成变量(例如IS的一部分)一起,地形变量(例如山体阴影)可以帮助解释该地区地表温度的大量空间变化(R-2 = 0.56-0.85)(p <0.001)。 “ IS的分数”变量的相对重要性也增加了,表明随着城市规模变大和SUHI变得越来越激烈,其有关地表温度空间变化的独特解释和预测能力也在增加。总体而言,这些结果表明,研究区域的凉爽温度并不位于山区,而不会阻碍SUHI的形成。因此,在为该地区的可持续城市发展进行景观规划时,应考虑UHI的形成和影响,包括可能的缓解和适应措施。 (C)2017国际摄影测量与遥感学会(ISPRS)。由Elsevier B.V.发布。保留所有权利。

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