改进的三层分解模型热红外影像空间降尺度研究
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  • 英文篇名:Spatial downscaling of thermal infrared image based on improved three-layer decomposition model
  • 作者:张文奇 ; 巩彩兰 ; 胡勇 ; 宋文韬 ; 匡定波
  • 英文作者:ZHANG Wen-Qi;GONG Cai-Lan;HU Yong;SONG Wen-Tao;KUANG Ding-Bo;Shanghai Institute of Technical Physics,Chinese Academy of Sciences;University of Chinese Academy of Sciences;Key Laboratory of Infrared System Detection and Imaging Tcchnology,Chinese Academy of Sciences;
  • 关键词:空间降尺度 ; 三层分解模型 ; 热红外影像 ; 地表温度
  • 英文关键词:spatial downscaling;;threelLayer decomposition;;thermal infrared image;;land surface temperature
  • 中文刊名:HWYH
  • 英文刊名:Journal of Infrared and Millimeter Waves
  • 机构:中国科学院上海技术物理研究所;中国科学院大学;中国科学院红外探测与成像技术重点实验室;
  • 出版日期:2019-04-15
  • 出版单位:红外与毫米波学报
  • 年:2019
  • 期:v.38
  • 基金:国家重点研发计划(2017YFC0602103);; 中科院上海技术物理研究所创新专项项目(CX-58)~~
  • 语种:中文;
  • 页:HWYH201902013
  • 页数:7
  • CN:02
  • ISSN:31-1577/TN
  • 分类号:73-79
摘要
地表温度(Land surface temperature,LST)是地-气相互作用和能量交换的重要参数之一.为了获取高空间分辨率地表温度数据,研究改进了一种热红外遥感数据降尺度方法,并以上海市Landsat8 OLI/TIRS影像为数据源进行了实验验证,归一化植被指数(Normalized Difference Vegetation Index,NDVI)被分解为低频层、边缘层和细节层,其中边缘层和细节层按比例增加到热红外数据中.并与经典的热红外降尺度方法 Dis Trad算法和Ts HARP算法作为对比,将模拟的地表温度(270 m)作为降尺度数据源实现LST降尺度(90 m).实验结果表明,三种降尺度方法都保留原有的地表温度的空间特征,但Dis Trad算法和Ts HARP算法增加了真实数据中并不存在的温度差异;改进的三层分解模型地表温度的均方根误差为0. 913 K,与Dis Trad方法和Ts HARP算法相比精度分别提高了0. 937 K和0. 832K.
        Land surface temperature is one of the important parameters of geogas interaction and energy exhange. In order to obtain the land surface temperature data with high spatial resolution,this research improved a method of downscaling thermal infrared remote image,and was verified using Shanghai Landsat 8 OLI/TIRS image as the data source. The Normalized Difference Vegetation Index( NDVI)was decomposed into lowfrequency layer,edge layer and detail layer,in which edge layer and detail layer are scaled up to the thermal infrared data. The proposed algorithm used simulated LST( 270 m) as a downscaling data source to achieve downscaling LST( 90 m),and compared with the classical thermal infrared downscaling method DisTrad algorithm and TsHARP algorithm. The results showthat all three downscaling methods preserve the spatial characteristics of the original land surface temperature,but the DisTrad algorithm and the TsHARP algorithm add the detailed information that does not exist in original land surface temperature data. The improved three-layers decomposition model has a root mean square error of 0. 913 K,which is 0. 937 K and 0. 832 K higher than the DisTrad method and the TsHARP method.
引文
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