Abstract The anisotropic scattering behavior of land surface is characterized by its bidirectional reflectance-distribution function (BRDF). However, a physically consistent BRDF definition is still lacking for heterogeneous and rugged terrain… Click to show full abstract
Abstract The anisotropic scattering behavior of land surface is characterized by its bidirectional reflectance-distribution function (BRDF). However, a physically consistent BRDF definition is still lacking for heterogeneous and rugged terrain that accounts for approximately 24% of Earth's land surface. In this study, we revisited current BRDF definitions and updated them for rugged terrain with few dependent parameters: illumination and viewing geometries, terrain shadows, effective areas of illumination and observation, and anisotropic reflectance properties of subpixel-scale slopes. Furthermore, the bidirectional reflectance factor (BRF), hemispherical-directional reflectance factor (HDRF), directional-hemispheric reflectance (DHR), and bi-hemispherical reflectance (BHR) were proposed within the current physical framework of reflectance quantities. These reflectance quantities have been adopted by the 3-D Discrete Anisotropic Radiative Transfer (DART) model to provide the simulations of remote sensing images. To highlight the importance of a proper usage of such reflectance terms, we used DART simulations to present the topographic effects on these reflectance quantities. Finally, the other issues with respect to surface BRDF/BRF, such as spatial scale of rugged terrain, characterization of anisotropic reflectance of micro-scale surfaces, derivative reflectance quantities, topographic parameters, wavelength dependence and reciprocity, and future perspective were discussed.
               
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