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国土资源遥感  2004, Vol. 16 Issue (3): 8-13    DOI: 10.6046/gtzyyg.2004.03.03
  技术方法 本期目录 | 过刊浏览 | 高级检索 |
基于DEM的ETM+图像辐射校正及汉江流域反照率的计算
朱叶飞1, 张万昌1, 蒋建军1,2
1. 南京大学国际地球系统科学研究所, 南京 210093;
2. 南京师范大学地理科学学院地图与遥感研究所, 南京 210097
RADIANT CORRECTION OF ETM+IMAGERY BASED ON DEM AND DERIVATION OF ALBEDO IN HANJIANG RIVER BASIN
ZHU Ye-fei1, ZHANG Wan-chang1, JIANG Jian-jun1,2
1. International Institute for Earth System Science, Nanking University, Nanjing 210093, China;
2. College of Geographical Science, Nanjing Normal University, Nanjing 210097, China
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摘要 对Gilabert[1]大气校正方法进行改进,提出了一种简单易行的辐射校正方法。该方法只需从ETM+图像上获取两个不同海拔高程的暗像元,再依据DEM进行大气校正,反演出各个高程上的大气及辐射参数,并在此基础上进行地形校正,进而获取LandsatETM+1~5和7波段的地表反射率,通过对各窄波段地表反射率的线性组合获取反照率。结果表明,该方法可行,精度较高。
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Abstract:This study presents an easy and fast radiant correction approach that can be used to perform atmospheric correction and topographic correction in mountain areas. This approach only needs the selection of two dark pixels in different elevations from ETM+ imagery, and the atmospheric correction based on DEM and dark pixels in different elevations can be conducted so as to get atmospheric and radiant parameters at all elevations. On such a basis, the topographic correction can be carried out and the surface reflectance can be calculated for ETM+ band 1~5 and 7. At last, a band integration approach is used to obtain the total continuous spectral albedo over the study site. The result shows that the method is effective in the inversion of surface albedo.
收稿日期: 2003-12-22      出版日期: 2011-08-02
基金资助:

国家重点基础研究发展规划项目(2001CB309404);杰出青年B类项目(40128001);教育部重点科学技术项目(2001)。

作者简介: 朱叶飞(1978-),男,硕士研究生,主要研究领域:遥感信息提取及遥感和GIS在水文学中的应用.
引用本文:   
朱叶飞, 张万昌, 蒋建军. 基于DEM的ETM+图像辐射校正及汉江流域反照率的计算[J]. 国土资源遥感, 2004, 16(3): 8-13.
ZHU Ye-fei, ZHANG Wan-chang, JIANG Jian-jun. RADIANT CORRECTION OF ETM+IMAGERY BASED ON DEM AND DERIVATION OF ALBEDO IN HANJIANG RIVER BASIN. REMOTE SENSING FOR LAND & RESOURCES, 2004, 16(3): 8-13.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2004.03.03      或      https://www.gtzyyg.com/CN/Y2004/V16/I3/8


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