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Titel |
Identification of potential rockfall source areas at a regional scale using a DEM-based geomorphometric analysis |
VerfasserIn |
A. Loye, M. Jaboyedoff, A. Pedrazzini |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1561-8633
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Digitales Dokument |
URL |
Erschienen |
In: Natural Hazards and Earth System Science ; 9, no. 5 ; Nr. 9, no. 5 (2009-10-08), S.1643-1653 |
Datensatznummer |
250006985
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Publikation (Nr.) |
copernicus.org/nhess-9-1643-2009.pdf |
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Zusammenfassung |
The availability of high resolution Digital Elevation Models (DEM) at a
regional scale enables the analysis of topography with high levels of detail.
Hence, a DEM-based geomorphometric approach becomes more accurate for
detecting potential rockfall sources. Potential rockfall source areas are
identified according to the slope angle distribution deduced from high
resolution DEM crossed with other information extracted from geological and
topographic maps in GIS format. The slope angle distribution can be
decomposed in several Gaussian distributions that can be considered as
characteristic of morphological units: rock cliffs, steep slopes, footslopes
and plains. A terrain is considered as potential rockfall sources when their
slope angles lie over an angle threshold, which is defined where the Gaussian
distribution of the morphological unit "Rock cliffs" become dominant over
the one of "Steep slopes". In addition to this analysis, the cliff outcrops
indicated by the topographic maps were added. They contain however "flat
areas", so that only the slope angles values above the mode of the Gaussian
distribution of the morphological unit "Steep slopes" were considered. An
application of this method is presented over the entire Canton of Vaud
(3200 km2), Switzerland. The results were compared with rockfall sources
observed on the field and orthophotos analysis in order to validate the
method. Finally, the influence of the cell size of the DEM is inspected by
applying the methodology over six different DEM resolutions. |
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