Multiple-scattering scheme useful for geometric optical modeling

被引:103
作者
Chen, JM [1 ]
Leblanc, SG
机构
[1] Univ Toronto, Dept Geog, Toronto, ON M5S 3G3, Canada
[2] Univ Toronto, Program Planning, Toronto, ON M5S 3G3, Canada
[3] Canada Ctr Remote Sensing, Ottawa, ON K1A 0Y7, Canada
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2001年 / 39卷 / 05期
关键词
directional remote sensing; geometrical optics (GOs); hyperspectral; multiple scattering; view factors;
D O I
10.1109/36.921424
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Geometrical optical (GO) models have been widely used in remote sensing applications because of their simplicity and ability to simulate angular variation of remote sensing signals from the earth's surface. GO models are generally accurate in the visible part of the solar spectrum, but less accurate in near-infrared (NIR) part in which multiple scattering in plant canopies is the strongest. Although turbid-media radiative transfer (RT) methods have been introduced to GO models to cope with the second-order and higher order scattering, the problem of canopy geometrical effects on multiple scattering still remains and becomes the main obstacle in GO model applications. In this paper, we propose and test a multiple scattering scheme to simulate angular variation in multiply scattered radiation in plant canopies, This scheme is based on various view factors between sunlit and shaded components (both foliage and background) in the canopy and allows the geometrical effects to propagate to the second-order and higher order scattering simulations. As the view factors depend on the canopy geometry, the scheme is particularly useful in GO models. This new scheme is implemented in the cl-Scale Model [4], which previously used band-specific multiple scattering factors. After the use of the scheme, these factors are removed and the multiple scatttering at a given wavelength and angle of observation can be automatically computed. Improvements made with this scheme are shown in comparison with the top-of-canopy (i.e., PARABOLA) and airborne (i.e., POLDER) measurements with modeled results with and without the scheme, Examples of canopy-level hyperspectral signatures simulated using the scheme are also shown.
引用
收藏
页码:1061 / 1071
页数:11
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