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(a) Bathymetric LiDAR measurement principle, (b) shaded relief map and water depth, (c) deposition and erosion of material due to a 30-year flood in the main channel and temporary side channels during the flood.

(a) Bathymetric LiDAR measurement principle, (b) shaded relief map and water depth, (c) deposition and erosion of material due to a 30-year flood in the main channel and temporary side channels during the flood.

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Conference Paper
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In this article the principle of laser scanning is recapitulated starting from the LiDAR equation and the measurement possibilities, especially beyond the range measurement, are explained. This includes the radiometric measurement, bathymetric LiDAR, waveform capturing, new possibilities from UAV platforms, and single photon counting detection. It...

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... hits the river or ocean ground surface, and travels the same way back to the sensor. Over dry land reflections are caused by surfaces. However, the different reflection properties at green light (e.g. 532nm) in comparison to the standard topographic wavelengths (e.g. 1064nm and 1550nm) need to be considered (see Fig. 1). As illustrated in Fig. 5, the river channel and the alluvial area can be acquired simultaneously with airborne laser scanning using a green LiDAR (Mandlburger et al., 2015a). This requires automatic classification of echoes into dry ground, wet ground, water surface, and vegetation (and other objects). This is intertwined with modeling of the water surface ...

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