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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >CALCULATIONS OF THE SOIL HOT-SPOT EFFECT USING THE COHERENT BACKSCATTERING THEORY
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CALCULATIONS OF THE SOIL HOT-SPOT EFFECT USING THE COHERENT BACKSCATTERING THEORY

机译:利用相干反散射理论计算土壤热斑效应

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The shadowing theory has been widely used to account for the hot-spot effect for the canopy and soil. However, it is not valid for soils that are composed of the particles and do not have well-defined shadows. The coherent backscattering theory is used in this study to calculate both the magnitude and the angular width of the hot-spot peak for clay and silt soils. The soil hot-spot magnitude is calculated by solving the vector radiative transfer equation. The dense nature of the soil medium is taken into account in the calculations of the hot-spot angular width. The results are also linked with the Hapke hot-spot empirical function. The effects of the wavelength dependence mid of particle size and shape also are examined. (C) Elsevier Science Inc., 1997. [References: 42]
机译:遮蔽理论已被广泛用于解释冠层和土壤的热点效应。但是,对于由颗粒组成且没有明确阴影的土壤无效。本研究采用相干反向散射理论来计算黏土和粉土的热点峰的大小和角宽。通过求解矢量辐射传递方程来计算土壤热点量。热点角宽的计算考虑了土壤介质的稠密性。结果也与Hapke热点经验函数相关。还检查了颗粒大小和形状的波长依赖性的影响。 (C)Elsevier Science Inc.,1997年。[参考:42]

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