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Study on the evolution tendency of the urban heat island effect in Xichang City using Remote Sensing

机译:基于遥感的西昌市城市热岛效应演变趋势研究

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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: ➀ 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; ➁ Before 2002, the built-up area expansion rate was 1.164hm2/a, and the increase rate of heat island intensity was 0.010°C/a. After 2002, they were 0.688hm2/a and 0.032°C/a respectively. ➂ 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.
机译:使用1995年7月31日,2002年8月27日和2007年9月18日获取的Landsat TM / ETM +图像,检索亮度温度。结合标准化归一化建筑指数(NDBI),监督分类和非监督分类方法从图像中提取建筑物区域。同时,计算它们的温度。计算了西昌市建成区的热岛强度;同时,利用城市热岛比率指数分析了城市热环境演变趋势。结果表明:➀按时间顺序,图像堆积面积分别为12.2 hm 2 ,20.35 hm 2 和23.79 hm 2 热岛强度分别为3.375℃,3.445℃和3.606℃。 2002 2002年以前,建筑面积扩张速度为1.164hm 2 / a,热岛强度增加速度为0.010°C / a。 2002年之后,分别为0.688hm 2 / a和0.032°C / a。 study研究区域的热岛比率指数分别为0.869、0.933和0.955。城市热岛效应总体呈上升趋势。

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