1. UTILISATION CONJOINTE DE TRAINS D'ONDES LIDAR VERT ET INFRAROUGE POUR LA BATHYMÉTRIE DES EAUX DE TRÈS FAIBLE PROFONDEURS.
- Author
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Allouis, Tristan, Bailly, Jean-Stéphane, Pastol, Yves, and Le Roux, Catherine
- Subjects
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TERRITORIAL waters , *SIGNAL processing , *BATHYMETRY - Abstract
Bathymetry and topography are crucial factors for the sustainable management of rivers and coastal areas. In this context, bathymetrie LiDAR appears as a useful technology for coastal and river mapping, offering an high spatial data density, an high acquisition rate and providing a continuous map between emerged and immersed area. Although some studies have investigated this technique's precision in moderately deep coastal areas, few have focused on very shallow waters (< 3 m). In this paper we introduce a new signal processing method for very shallow waters bathymetry. The methods is based on a simultaneous process of green and near-infrared (NIR) LiDAR waveforms. We then evaluate the density and accuracy of the resulting estimations of very shallow waters bathymetry. In this paper, we present our work on a dataset from the Golfe du Morbihan, France, acquired by SHOM (French Navy Hydrographic and Oceanographic Service) in 2005 with a SHOALS system providing Raman, NIR, and green LiDAR waveforms. This work focuses on the data quality resulting from two different processing methods using near-infrared and green signals for surface and water bottom topography: the delivered data processed method and the proposed algorithm. In order to perform a better comparison of altimetrical data between GPS ground control points (pinpoints) and LiDAR footprints(diameter around 2 m), we also used a specific aggregation method (MAUP). In selected very shallow areas, we show that our algorithm extracts 41% of additional measurements from initially delivered data with a similar bias (around 5 cm) and a lower standard deviation of errors (26.1 cm vs. 41.1 cm). 55% of theses additional points are located between 1.5 m and 2 m and our algorithm can detect depths 80 cm shallower than the delivered data (1 m vs. 1.8 m). [ABSTRACT FROM AUTHOR]
- Published
- 2017
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