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Titel Improvement of snow avalanche hazard and vulnerability assessment in the French Alps using a combination of dendrogeomorphic and statistical approachs
VerfasserIn Romain Schläppy, Vincent Jomelli, Markus Stoffel, Delphine Grancher, Michael Deschatres, Daniel Brunstein
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250046392
 
Zusammenfassung
Snow avalanches constitute major threats for human activities, settlements and infrastructure in mountain environments. In a context of constant demographic growth populations tend to build closer to areas influenced by natural hazards. In the Chamonix region (France), for instance, twelve persons were killed by an extreme snow avalanche in 1999. Such high magnitude snow avalanches are relatively rare but of interest for research and administration since they correspond to those which can potentially affect human infrastructure and their residents. Probabilistic models have been used in the past to determine snow avalanche extent of extreme events based on e.g., release and run-out altitudes or topographical characteristics. In France, such data is compiled by CEMAGREF in a database called EPA (Enquête Permanente sur les Avalanches) which contains information on ~70,000 events from 4400 avalanche sites since AD 1900. The database contains a huge number of historical accounts on past avalanche events but lacks accuracy as one goes back in time. In fact, stringent rules for a complete recording of event characteristics have only been implemented in 2001. A real need for empirical data therefore exists to compare and complement archival records with additional quantitative information. Dendrogeomorphology appears to be an appropriate tool to close the data gap and to provide field evidence for past avalanches and consecutively for the spatio-temporal reconstruction of high magnitude avalanche events. As part of the national research project MOPERA, aiming at the improvement of snow avalanche and vulnerability assessment in France, we use dendrogeomorphic techniques to analyze three avalanche paths in the French Alps. Results of this study will yield additional details to existing historical data on run-out distance, extent and return periods of extreme avalanche events. Furthermore they will be confronted with outcomes of the statistical dynamical simulations performed by CEMAGREF. In addition, we will try to identify climatic variables favoring the release of high magnitude avalanches.