Abstract

The original intensity value recorded by terrestrial laser scanners is influenced by multiple variables, among which incidence angle and distance play a crucial and dominant role. Further studies on incidence angle and distance effects are required to improve the accuracy of currently available methods and to implement these methods in practical applications. In this study, the effects of incidence angle and distance on intensity data of the Faro Focus3D 120 terrestrial laser scanner are investigated. A new method is proposed to eliminate the incidence angle and distance effects. The proposed method is based on the linear interpolation of the intensity values of reference targets previously scanned at various incidence angles and distances. Compared with existing methods, a significant advantage of the proposed method is that estimating the specific function forms of incidence angle versus intensity and distance versus intensity is no longer necessary; these are canceled out when the scanned and reference targets are measured at the same incidence angle and distance. Results imply that the proposed method has high accuracy and simplicity in eliminating incidence angle and distance effects and can significantly reduce the intensity variations caused by these effects on homogeneous surfaces.

Highlights

  • Terrestrial laser scanning (TLS), a revolutionary technique for the acquisition of spatial data, has gained widespread acceptance in both scientific and commercial communities as a powerful tool for topographic measurement in various geophysical disciplines in the last two decades [1]

  • The distances and incidence angles were calculated according to Equation (24)

  • We discussed the effects of incidence angle and distance on TLS intensity measurements of the

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Summary

Introduction

Terrestrial laser scanning (TLS), a revolutionary technique for the acquisition of spatial data, has gained widespread acceptance in both scientific and commercial communities as a powerful tool for topographic measurement in various geophysical disciplines in the last two decades [1] This active remote sensing technique allows for the direct and illumination-independent measurement of 3-D objects in a fast, contactless, non-destructive, and accurate manner [2] by emitting monochromatic beams of light mostly in the near-infrared region of the electromagnetic spectrum. Apart from discrete topography measurements, almost all current TLS instruments simultaneously measure the power of the backscattered laser signal of each point and record it as an intensity value [3].

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