2010
DOI: 10.1117/12.851978
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Predicted bathymetric lidar performance of Coastal Zone Mapping and Imaging Lidar (CZMIL)

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Cited by 13 publications
(10 citation statements)
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“…This pre-analysis classification is important because bathymetric and topographic lidar waveforms have different characteristics and are dealt with differently 3 In the figure, we show cases of clean targets and multiple targets. Clean targets arise from bare land, large roof tops and walls of buildings etc.…”
Section: Algorithm Development: Peak Detectionmentioning
confidence: 98%
See 1 more Smart Citation
“…This pre-analysis classification is important because bathymetric and topographic lidar waveforms have different characteristics and are dealt with differently 3 In the figure, we show cases of clean targets and multiple targets. Clean targets arise from bare land, large roof tops and walls of buildings etc.…”
Section: Algorithm Development: Peak Detectionmentioning
confidence: 98%
“…By computing ranges from the simulated waveforms, we can generate a direct comparison to ranges generated in the simulator. We made every effort to use realistic (even pessimistic) simulated CZMIL waveforms 3 . Therefore, we believe the ranging procedure discussed and the accuracies determined in the simulation are representative of what we expect in actual CZMIL data (when it comes available).…”
Section: Experiments With Simulated Datamentioning
confidence: 99%
“…Then, using the position and orientation data for the aircraft, and the pointing information from the lidar, we compute 3D ellipsoid coordinates on the land/sea surface and the seafloor. The resulting products are the sea floor lidar point cloud in ellipsoid heights and the land/sea surface point cloud in ellipsoid heights (h s and h b ) [3][4] . The water depth, D, is then computed as the difference between the two surfaces defined by the point clouds.…”
Section: Level 2 Processor: Flightline-based Auto-processor and Auto-mentioning
confidence: 99%
“…Equation (1) can also represent the optical domain signal detected from arbitrary depth D by replacing ρ with β π (the water backscattering coefficient) and by treating the stretch factor as unity. The latter representation is often called the water column response [4]. Together, the water column response and the sea floor response form two parts of a piecewise function that characterizes the returned signal at any depth.…”
Section: Theory and Backgroundmentioning
confidence: 99%