首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Across-path DN gradient in Landsat TM imagery of Amazonian forests: A challenge for image interpretation and mosaicking
【24h】

Across-path DN gradient in Landsat TM imagery of Amazonian forests: A challenge for image interpretation and mosaicking

机译:亚马逊森林Landsat TM影像中的跨径DN梯度:影像解释和镶嵌的挑战

获取原文
获取原文并翻译 | 示例
           

摘要

An analysis of tropical rain forest covering Amazonian lowlands has highlighted a systematic across-path, east-west radiometric gradient within Landsat TM imagery. Visual assessment of 45 and quantitative analysis of 20 Amazonian Landsat-4 and -5 TM scenes show that the gradient is band dependent and pronounced in visible light bands I to 3 but significant also in IR bands 4 to 7. The results show that the scan line location of a pixel explains a considerable amount of the DN variation of forests in the width of the entire scene (B1: 70%, 132: 52%, 133: 44%, 134: 34%, 135: 46%, B7: 39%). In digital numbers, the difference between east and west side of a scene may be small (9, 4, 3, 10, 9, 3, respectively) but these differences become significant if the images are to be mosaicked, or the data are used for mapping relatively subtle differences of natural forests. Apparently, the gradient is a result of at least three factors: 1) shadows caused by the undulating terrain, 2) anisotropic reflectance of the varying surfaces, and 3) atmospheric scattering. The phenomenon becomes more significant when the sun is high and the scanning line is close to solar azimuth direction-a. condition more easily encountered in lower latitudes of the earth. (c) 2005 Elsevier Inc. All rights reserved.
机译:对覆盖亚马逊低地的热带雨林进行的分析突出显示,Landsat TM影像内有系统的跨路径,东西向辐射梯度。对45个图像进行视觉评估并对20个Amazon Landsat-4和-5 TM场景进行定量分析,结果表明该梯度与波段有关,并且在可见光波段I至3中明显,但在红外波段4至7中也很明显。结果表明,扫描像素的线位置可以解释整个场景宽度中森林的DN差异(B1:70%,132:52%,133:44%,134:34%,135:46%,B7: 39%)。在数字中,场景的东侧和西侧之间的差异可能很小(分别为9、4、3、10、9、3),但是如果要镶嵌图像或使用数据,则这些差异会变得很明显。用于绘制天然森林相对细微的差异。显然,该梯度是至少三个因素的结果:1)起伏的地形造成的阴影; 2)不同表面的各向异性反射率; 3)大气散射。当太阳高且扫描线接近太阳方位角-a时,该现象变得更加明显。在地球的低纬度地区更容易遇到这种情况。 (c)2005 Elsevier Inc.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号