Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XXXIX-B5, 511-516, 2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
30 Jul 2012
D. Hoffmeister1, N. Tilly1, C. Curdt1, H. Aasen1, K. Ntageretzis2, H. Hadler2, T. Willershäuser2, A. Vött2, and G. Bareth1 1Institute of Geography, University of Cologne, Albertus-Magnus-Platz, 50923 Cologne, Germany
2Institute of Geography, Johannes Gutenberg-University Mainz, Johann-Joachim-Becher-Weg 21, 55099 Mainz, Germany
Keywords: TLS, Multitemporal, Geomorphology, Coast, Hazards, History Abstract. We used terrestrial laser scanning (TLS) for (i) accurate volume estimations of dislocated boulders moved by high-energy impacts and for (ii) monitoring of annual coastal changes. In this contribution, we present three selected sites in Western Greece that were surveyed during a time span of four years (2008-2011). The Riegl LMS-Z420i laser scanner was used in combination with a precise DGPS system (Topcon HiPer Pro). Each scan position and a further target were recorded for georeferencing and merging of the point clouds. For the annual detection of changes, reference points for the base station of the DGPS system were marked.
Our studies show that TLS is capable to accurately estimate volumes of boulders, which were dislocated and deposited inland from the littoral zone. The mass of each boulder was calculated from this 3D-reconstructed volume and according density data. The masses turned out to be considerably smaller than common estimated masses based on tape-measurements and according density approximations. The accurate mass data was incorporated into wave transport equations, which estimate wave velocities of high-energy impacts. As expected, these show smaller wave velocities, due to the incorporated smaller mass.
Furthermore, TLS is capable to monitor annual changes on coastal areas. The changes are detected by comparing high resolution digital elevation models from every year. On a beach site, larger areas of sea-weed and sandy sediments are eroded. In contrast, bigger gravel with 30-50 cm diameter was accumulated. At the other area with bigger boulders and a different coastal configuration only slightly differences were detectable.
In low-lying coastal areas and along recent beaches, post-processing of point clouds turned out to be more difficult, due to noise effects by water and shadowing effects. However, our studies show that the application of TLS in different littoral settings is an appropriate and promising tool. The combination of both instruments worked well and the annual positioning procedure with own survey point is precose for this purpose.

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Citation: Hoffmeister, D., Tilly, N., Curdt, C., Aasen, H., Ntageretzis, K., Hadler, H., Willershäuser, T., Vött, A., and Bareth, G.: TERRESTRIAL LASER SCANNING FOR COASTAL GEOMORPHOLOGIC RESEARCH IN WESTERN GREECE, Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XXXIX-B5, 511-516, doi:10.5194/isprsarchives-XXXIX-B5-511-2012, 2012.

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