2020
DOI: 10.3390/s20072063
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Aerial Laser Scanning Data as a Source of Terrain Modeling in a Fluvial Environment: Biasing Factors of Terrain Height Accuracy

Abstract: Airborne light detection and ranging (LiDAR) scanning is a commonly used technology for representing the topographic terrain. As LiDAR point clouds include all surface features present in the terrain, one of the key elements for generating a digital terrain model (DTM) is the separation of the ground points. In this study, we intended to reveal the efficiency of different denoising approaches and an easy-to-use ground point classification technique in a floodplain with fluvial forms. We analyzed a point cloud … Show more

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Cited by 11 publications
(6 citation statements)
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“…As demonstrated in [ 68 ], cloud pre-filtration is very important and enables the isolation of vital infrastructure elements. Pre-filtration was also applied in [ 69 ]. Pre-filtration consists of four stages: noise filtering, cloth simulation filtering [ 70 ] (CSF), data reduction and statistical outlier removal (SOR) filtering.…”
Section: Methodsmentioning
confidence: 99%
“…As demonstrated in [ 68 ], cloud pre-filtration is very important and enables the isolation of vital infrastructure elements. Pre-filtration was also applied in [ 69 ]. Pre-filtration consists of four stages: noise filtering, cloth simulation filtering [ 70 ] (CSF), data reduction and statistical outlier removal (SOR) filtering.…”
Section: Methodsmentioning
confidence: 99%
“…For generating the grids, we selected the natural neighbor interpolation method with ground belonging to the DSM [59]. This choice was in line with recent studies [60], proving that this interpolation method yields the most accurate models. Finally, we clipped regular grids corresponding to Sites 1 and 2 from the CHM and the DSM.…”
Section: Datamentioning
confidence: 97%
“…The wetland areas #b1 and #b2 in Figure 9 were also oxbow lakes, but in the next phase of the succession, the proportion of open water was lower, and according to the CLC classification, these lakes were interpreted as wetlands (as these smaller lakes can run dry during dry summers [67], the classification can be accepted). The wetland area #b3 ( Figure 9) was a set of swales and point bars (i.e., negative and positive fluvial forms) with different water cover and height of vegetation, where the reflectance pattern can be similar both to grasslands and eutrophic lakes [68,69]. The wetland area #b4 (Figure 9) was also a set of swales and point bars (consisting of two different parts, of which the northern part was the older with transformed forms), while the fifth wetland area (Figure 9/b5) was a floodplain lake with its surroundings (open water with aquatic vegetation and marshlands).…”
Section: Clc Classes and The Mixture Of Spectral Featuresmentioning
confidence: 99%