Modeling the Reflectance of the Lunar Regolith by a New Method Combining Monte Carlo Ray Tracing and Hapke’s Model with Application to Chang’E-1 IIM Data
Figure 20
The 2D results of removing the influence of the topography applying our model. (a) profile of CE-1 IIM data (nm); (b) diffusion intensity calculated by CE-1 elevation map of the same region; (c) result obtained by using the inverse process of our method to CE-1 IIM data.
