摘要
基于2004、2009、2013年的Landsat系列遥感影像,应用单窗算法反演武夷山市相应时点的地表温度,采用均值-标准差法对地表温度反演结果进行分级.结果表明:武夷山市的地表温度分布呈现出由市区中心向四周逐渐降低的趋势,市区主要交通干线及其周围一定区域内地表温度较高,距离交通干线越远,地表温度越低;2004-2013年武夷山市高温区域面积扩大,热岛效应逐步增强.
Based on a series of Landsat remote sensing imagery of 2004, 2009 and 2013, LST(Land Surface Temperature ) of Wuyishan city during the 3 years was retrieved by Qin Zhi-hao ’ s Mono-window Algorithm and the result was classified by average-standard deviation .The results showed that the surface temperature of Wuyishan city reduced gradually from city center to the surrounding areas ; from the changing characteristics it could be seen that the LST in the main traffic arteries and its surroundings were higher than the other areas ;the farther the distance from the traffic route , the lower the temperature would be .Compared with the former two LST results, there was a wider area of high temperature in 2013.From the year 2004 to 2013, the high temperature area in Wuyishan city had expanded to a certain degree , and the urban heat island effect had become more serious than before .
出处
《吉林师范大学学报(自然科学版)》
2015年第3期152-156,共5页
Journal of Jilin Normal University:Natural Science Edition
基金
国家自然科学基金项目(J1210067)
福建省科技重大专项(2012NZ0002-1-5)
福建省大学生创新创业训练计划项目(cxxl-2014108)
关键词
地表温度
LANDSAT
单窗算法
武夷山市
Landsat
land surface temperature
Landsat
mono-window algorithm
Wuyishan city