首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Seeing through shadow: Modelling surface irradiance for topographic correction of Landsat ETM+ data
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Seeing through shadow: Modelling surface irradiance for topographic correction of Landsat ETM+ data

机译:透视阴影:建模表面辐照度以对Landsat ETM +数据进行地形校正

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Despite advances in remote sensing, retrieving surface properties at high resolutions in complex terrain is a major challenge. Slope and aspect as well as the topography surrounding a target impact surface insolation and lead to variability in calculated surface reflectance even for homogeneous land cover. Retrieval of surface reflectance is particularly problematic in case of topographic shading, where the total irradiation at the surface is a combination of diffuse irradiation and terrain-reflected irradiation from nearby slopes. To facilitate the retrieval of surface reflectance from high-resolution optical remote sensing, we have explored the feasibility of using a three dimensional radiative transfer code to simulate gridded surface irradiance for a ~ 37 km~2 area in the New Zealand Southern Alps. We have tested the sensitivity of simulated irradiance and calculated surface reflectance both in- and outside shaded areas to atmospheric aerosol content, surface albedo, atmospheric boundary layer structure and different solar spectra. Retrieved surface reflectance has been shown to be highly sensitive to atmospheric aerosols and surface albedo, particularly for areas shaded by topography. Not considering atmospheric aerosols in topographic correction can increase derived surface reflectance by well over 50%, while terrain-reflected irradiance can contribute 40% to surface reflectance in shaded areas, even for wider valleys. Both factors should therefore be considered in topographic correction of satellite imagery, even for relatively aerosol-free atmospheres and low surface albedo. Topographic correction for the whole scene was performed with the model settings resulting in the smallest RMSD between surface reflectivity in shaded and unshaded areas of similar land cover. Topographic correction based on 3D radiative transfer simulations has proven to effectively remove topographic effects and almost equalise derived mean reflectance in- and outside shaded areas. While the effective removal of shadows likely requires a higher dynamic range than Land-sat's ETM+ can offer, we suggest further evaluation of this approach in future studies at other sites and with other sensors.
机译:尽管遥感技术取得了进步,但在复杂地形中以高分辨率检索表面属性仍然是一项重大挑战。即使是均匀的土地覆被,目标目标表面周围的坡度,坡向以及地形也会影响其表面反射率,并导致计算出的表面反射率发生变化。在地形阴影的情况下,表面反射率的检索尤其成问题,其中表面处的总照射是来自附近斜坡的漫射照射和地形反射照射的组合。为了方便从高分辨率光学遥感中检索表面反射率,我们探索了使用三维辐射转移码来模拟新西兰南阿尔卑斯山〜37 km〜2地区的网格化表面辐照度的可行性。我们已经测试了模拟辐照度的敏感度,并计算了阴影内外区域对大气气溶胶含量,表面反照率,大气边界层结构和不同太阳光谱的表面反射率的敏感性。检索到的表面反射率已显示出对大气气溶胶和表面反照率高度敏感,特别是对于地形遮蔽的区域。在地形校正中不考虑大气气溶胶可以使得出的表面反射率提高50%以上,而在倾斜区域,即使在更宽的山谷中,地形反射的辐照度也可以使表面反射率贡献40%。因此,即使在相对无气溶胶的大气和低地表反照率的情况下,在卫星图像的地形校正中也应考虑这两个因素。使用模型设置对整个场景进行地形校正,从而在相似土地覆盖的阴影和非阴影区域中,在表面反射率之间的最小RMSD。已经证明,基于3D辐射转移模拟的地形校正可以有效消除地形影响,并使阴影区域内外的平均反射率几乎相等。虽然有效去除阴影可能需要比Land-sat的ETM +所能提供的动态范围更大的动态范围,但我们建议在将来在其他站点和其他传感器上进行研究时,对该方法进行进一步评估。

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