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 16
Simulation results of the location based distribution of the minerals (sample rate = 1000, size: ). (a) the reflectance of the distribution of the samples; (b) final result of the terrain with diffusion.
