“…This DN, which represents the back scattered signal, is mainly a function of some important physical quantities, such as the direction of the light source with respect to the observed object, i.e., the direction of the incident energy, the distance from the object, the wavelength used, the surface reflectance, the thermo-hygrometric conditions of the electromagnetic wave propagation medium and the proximity of the affected object to other highly reflective bodies [10]. Return wave intensity measurements were mainly used to support the visual analysis of a point cloud and also for different applications, such as for orientation [11], recording [12], manual inspection of trees [13], rock face investigation [14] or classification based on the surface material properties [15,16].…”