基于遥感的西昌市城市热岛效应演变趋势研究

Chuanhong Zhang, Huixi Xu
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引用次数: 1

摘要

利用1995年7月31日、2002年8月27日和2007年9月18日的Landsat TM/ETM+影像反演了该地区的亮度温度。采用归一化差分建筑指数(NDBI)、监督分类和非监督分类相结合的方法从图像中提取建成区。同时,计算了它们的温度。对西昌市建成区热岛强度进行了计算;同时,利用城市热岛比指数分析了城市热环境的演变趋势。结果表明:(1)从时序上看,建成区面积分别为12.2 hm2、20.35 hm2和23.79 hm2,热岛强度分别为3.375℃、3.445℃和3.606℃;(2) 2002年以前,建成区面积扩张率为1.164 hm2/a,热岛强度增长率为0.010℃/a。2002年以后分别为0.688 hm2/a和0.032℃/a。(3)研究区热岛比指数分别为0.869、0.933和0.955。城市热岛效应总体呈上升趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the evolution tendency of the urban heat island effect in Xichang City using Remote Sensing
Using Landsat TM/ETM+ images acquired on July 31, 1995, August 27, 2002, and September 18, 2007, the brightness temperature was retrieved. Built-up areas were extracted from images by combining normalized difference building index (NDBI), supervised classification, and unsupervised classification method. Meanwhile, their temperature was calculated. The heat island intensity of built-up area in Xichang City was calculated; simultaneously, the city thermal environment evolution trend was analyzed by using the urban heat island ratio index. The results show that: (1) Chronologically according to the images, the built-up area were 12.2 hm2, 20.35 hm2 and 23.79 hm2 respectively, and the heat island intensity were 3.375 °C, 3.445 °C, and 3.606, °C respectively; (2) Before 2002, the built-up area expansion rate was 1.164 hm2/a, and the increase rate of heat island intensity was 0.010°C/a. After 2002, they were 0.688 hm2/a and 0.032°C/a respectively. (3) the heat island ratio index in study area were 0.869, 0.933, and 0.955, respectively. The Urban Heat Island Effects showed an overall upward trend.
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