2020
DOI: 10.36783/18069657rbcs20200076
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Sediment source and volume of soil erosion in a gully system using UAV photogrammetry

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Cited by 9 publications
(5 citation statements)
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References 44 publications
(56 reference statements)
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“…The plugin allows direct comparison of point clouds and detects changes with very little manual work. The algorithm is described in several papers (e.g., [32,[68][69][70][71][72]), but the working principle is to find the most appropriate normal direction for points and calculate the distances between point clouds along a cylinder of a given diameter (the projection scale), projected along the normal. The normal scale was defined as 25 times the average local roughness calculated for a point cloud by the CloudCompare, in accordance with the work of Ferrer-González et al [71].…”
Section: Assessment Of Errorsmentioning
confidence: 99%
“…The plugin allows direct comparison of point clouds and detects changes with very little manual work. The algorithm is described in several papers (e.g., [32,[68][69][70][71][72]), but the working principle is to find the most appropriate normal direction for points and calculate the distances between point clouds along a cylinder of a given diameter (the projection scale), projected along the normal. The normal scale was defined as 25 times the average local roughness calculated for a point cloud by the CloudCompare, in accordance with the work of Ferrer-González et al [71].…”
Section: Assessment Of Errorsmentioning
confidence: 99%
“…), using the Multiscale Model to Model Cloud Comparison (M3C2) algorithm. The M3C2 algorithm was already successfully applied for point cloud-based detection of STCs caused by various geomorphic processes, such as river dynamics [50], soil erosion [27,[51][52][53], rockfalls [12,54], rock glaciers [54][55][56], etc. Since the M3C2 algorithm is a point cloud-based method, it allows detection of complex (3D) soil erosion induced STCs, thus successfully overcoming the shortcomings of DEMs of difference (DoDs) related to the complex morphology of erosional forms [51,52,57].…”
Section: Detection Of Spatio-temporal Changes Within Gully Headcutmentioning
confidence: 99%
“…The M3C2 algorithm was already successfully applied for point cloud-based detection of STCs caused by various geomorphic processes, such as river dynamics [50], soil erosion [27,[51][52][53], rockfalls [12,54], rock glaciers [54][55][56], etc. Since the M3C2 algorithm is a point cloud-based method, it allows detection of complex (3D) soil erosion induced STCs, thus successfully overcoming the shortcomings of DEMs of difference (DoDs) related to the complex morphology of erosional forms [51,52,57]. As DoD represents a 2.5D model, significant errors can occur during the detection of STCs, especially in complex steep and overhanging parts of the terrain where 2.5D models cannot accurately represent the terrain morphology [50,[58][59][60].…”
Section: Detection Of Spatio-temporal Changes Within Gully Headcutmentioning
confidence: 99%
“…UAVs are commonly used in topographic change detection applications thanks to the newly emerged techniques and sensor evolution, resulting in highly efficient data acquisition [58,59]. This advanced and cost-effective technology has led to multiple research applications concerning landscape analysis and erosive process estimation [60][61][62][63]. The use of Structure-from-Motion (SfM) and multi-view stereopsis (MVS) enhances the capability of transforming a large number of overlapping images into 3D point clouds, Digital Terrain Models (DTM) and orthomosaics, even at mm-level accuracy [49,[64][65][66][67].…”
Section: Introductionmentioning
confidence: 99%