Landslide detection and monitoring capability of boat-based mobile laser scanning along Dieppe coastal cliffs, Normandy

被引:0
|
作者
Clément Michoud
Dario Carrea
Stéphane Costa
Marc-Henri Derron
Michel Jaboyedoff
Christophe Delacourt
Olivier Maquaire
Pauline Letortu
Robert Davidson
机构
[1] University of Lausanne,Institute of Earth Sciences
[2] Universit de Caen Basse-Normandie,LETG
[3] Université de Bretagne Occidentale,CAEN GEOPHEN
[4] Terr@num,LDO, UMR 6538
来源
Landslides | 2015年 / 12卷
关键词
Mobile laser scanning; Coastline change detection; Rockfall; Landslide monitoring; High Normandy coastal cliffs;
D O I
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中图分类号
学科分类号
摘要
Integrated in a wide research assessing destabilizing and triggering factors to model cliff dynamic along the Dieppe’s shoreline in High Normandy, this study aims at testing boat-based mobile LiDAR capabilities by scanning 3D point clouds of the unstable coastal cliffs. Two acquisition campaigns were performed in September 2012 and September 2013, scanning (1) a 30-km-long shoreline and (2) the same test cliffs in different environmental conditions and device settings. The potentials of collected data for 3D modelling, change detection and landslide monitoring were afterward assessed. By scanning during favourable meteorological and marine conditions and close to the coast, mobile LiDAR devices are able to quickly scan a long shoreline with median point spacing up to 10 cm. The acquired data are then sufficiently detailed to map geomorphological features smaller than 0.5 m2. Furthermore, our capability to detect rockfalls and erosion deposits (>m3) is confirmed, since using the classical approach of computing differences between sequential acquisitions reveals many cliff collapses between Pourville and Quiberville and only sparse changes between Dieppe and Belleville-sur-Mer. These different change rates result from different rockfall susceptibilities. Finally, we also confirmed the capability of the boat-based mobile LiDAR technique to monitor single large changes, characterizing the Dieppe landslide geometry with two main active scarps, retrogression up to 40 m and about 100,000 m3 of eroded materials.
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页码:403 / 418
页数:15
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    [J]. LANDSLIDES, 2015, 12 (02) : 403 - 418
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